Articles | Volume 20, issue 11
https://doi.org/10.5194/bg-20-2161-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-20-2161-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Jun 2023
Research article |
| 15 Jun 2023
| 15 Jun 2023
Examination of the parameters controlling the triple oxygen isotope composition of grass leaf water and phytoliths at a Mediterranean site: a model–data approach
Aix-Marseille Université, CNRS, IRD, INRAE, CEREGE, 13545
Aix-en-Provence, France
present address: Department of Biology and
Geology, University of Almería, 04120 Cañada de San Urbano, Almería, Spain
Aix-Marseille Université, CNRS, IRD, INRAE, CEREGE, 13545
Aix-en-Provence, France
Ilja M. Reiter
Research Federation ECCOREV, FR3098, CNRS, 13545 Aix-en-Provence,
France
Jean-Philippe Orts
IMBE, CNRS, Université d'Avignon, Aix-Marseille Université,
IRD, 13397 Marseille, France
Christine Vallet-Coulomb
Aix-Marseille Université, CNRS, IRD, INRAE, CEREGE, 13545
Aix-en-Provence, France
Clément Piel
ECOTRON Européen de Montpellier, UAR 3248, CNRS, Campus de
Baillarguet, 34980 Montferrier-sur-Lez, France
Jean-Charles Mazur
Aix-Marseille Université, CNRS, IRD, INRAE, CEREGE, 13545
Aix-en-Provence, France
Julie C. Aleman
Aix-Marseille Université, CNRS, IRD, INRAE, CEREGE, 13545
Aix-en-Provence, France
Corinne Sonzogni
Aix-Marseille Université, CNRS, IRD, INRAE, CEREGE, 13545
Aix-en-Provence, France
Helene Miche
Aix-Marseille Université, CNRS, IRD, INRAE, CEREGE, 13545
Aix-en-Provence, France
Jérôme Ogée
INRAE, Bordeaux Sciences Agro, UMR ISPA, 33140 Villenave-d'Ornon,
France
Related authors
Claudia Voigt, Fernando Gázquez, Lucía Martegani, Ana Isabel Sánchez Villanueva, Antonio Medina, Rosario Jiménez-Espinosa, Juan Jiménez-Millán, and Miguel Rodríguez-Rodríguez
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-290, https://doi.org/10.5194/hess-2024-290, 2024
Preprint under review for HESS
Short summary
Short summary
This research explores the use of a new isotope tracer, 17O-excess, to better understand how hydrological processes drive large seasonal water level changes in small lakes in semiarid regions. The study shows that triple oxygen isotopes offer a more detailed understanding of these changes compared to traditional methods. These findings are valuable for reconstructing past climates and predicting how climate change, influenced by human activity, will affect small lakes in these dry areas.
Clément Outrequin, Anne Alexandre, Christine Vallet-Coulomb, Clément Piel, Sébastien Devidal, Amaelle Landais, Martine Couapel, Jean-Charles Mazur, Christophe Peugeot, Monique Pierre, Frédéric Prié, Jacques Roy, Corinne Sonzogni, and Claudia Voigt
Clim. Past, 17, 1881–1902, https://doi.org/10.5194/cp-17-1881-2021, https://doi.org/10.5194/cp-17-1881-2021, 2021
Short summary
Short summary
Continental atmospheric humidity is a key climate parameter poorly captured by global climate models. Model–data comparison approaches that are applicable beyond the instrumental period are essential to progress on this issue but face a lack of quantitative relative humidity proxies. Here, we calibrate the triple oxygen isotope composition of phytoliths as a new quantitative proxy of continental relative humidity suitable for past climate reconstructions.
Claudia Voigt, Daniel Herwartz, Cristina Dorador, and Michael Staubwasser
Hydrol. Earth Syst. Sci., 25, 1211–1228, https://doi.org/10.5194/hess-25-1211-2021, https://doi.org/10.5194/hess-25-1211-2021, 2021
Short summary
Short summary
Evaporation trends in the stable isotope composition (18O/16O, 17O/16O, 2H/1H) of throughflow ponds in a hydrologically complex and seasonally dynamic lake system can be reliably predicted by the classic Craig–Gordon isotope evaporation model. We demonstrate that the novel 17O-excess parameter is capable of resolving different types of evaporation with and without recharge and of identifying mixing processes that cannot be resolved using the classic δ2H–δ18O system alone.
Claudia Voigt, Fernando Gázquez, Lucía Martegani, Ana Isabel Sánchez Villanueva, Antonio Medina, Rosario Jiménez-Espinosa, Juan Jiménez-Millán, and Miguel Rodríguez-Rodríguez
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-290, https://doi.org/10.5194/hess-2024-290, 2024
Preprint under review for HESS
Short summary
Short summary
This research explores the use of a new isotope tracer, 17O-excess, to better understand how hydrological processes drive large seasonal water level changes in small lakes in semiarid regions. The study shows that triple oxygen isotopes offer a more detailed understanding of these changes compared to traditional methods. These findings are valuable for reconstructing past climates and predicting how climate change, influenced by human activity, will affect small lakes in these dry areas.
Maëlie Chazette, Patrick Chazette, Ilja M. Reiter, Xiaoxia Shang, Julien Totems, Jean-Philippe Orts, Irène Xueref-Remy, and Nicolas Montes
Biogeosciences, 21, 3289–3303, https://doi.org/10.5194/bg-21-3289-2024, https://doi.org/10.5194/bg-21-3289-2024, 2024
Short summary
Short summary
The approach presented is original in its coupling between field observations and airborne lidar observations. It has been applied to an instrumented reference forest site in the south of France, which is heavily impacted by climate change. It leads to the evaluation of tree heights and ends with assessments of aerial and root carbon stocks. A detailed assessment of uncertainties is presented to add a level of reliability to the scientific products delivered.
Philip Meister, Anne Alexandre, Hannah Bailey, Philip Barker, Boris K. Biskaborn, Ellie Broadman, Rosine Cartier, Bernhard Chapligin, Martine Couapel, Jonathan R. Dean, Bernhard Diekmann, Poppy Harding, Andrew C. G. Henderson, Armand Hernandez, Ulrike Herzschuh, Svetlana S. Kostrova, Jack Lacey, Melanie J. Leng, Andreas Lücke, Anson W. Mackay, Eniko Katalin Magyari, Biljana Narancic, Cécile Porchier, Gunhild Rosqvist, Aldo Shemesh, Corinne Sonzogni, George E. A. Swann, Florence Sylvestre, and Hanno Meyer
Clim. Past, 20, 363–392, https://doi.org/10.5194/cp-20-363-2024, https://doi.org/10.5194/cp-20-363-2024, 2024
Short summary
Short summary
This paper presents the first comprehensive compilation of diatom oxygen isotope records in lake sediments (δ18OBSi), supported by lake basin parameters. We infer the spatial and temporal coverage of δ18OBSi records and discuss common hemispheric trends on centennial and millennial timescales. Key results are common patterns for hydrologically open lakes in Northern Hemisphere extratropical regions during the Holocene corresponding to known climatic epochs, i.e. the Holocene Thermal Maximum.
Jérôme Texier, Julio Gonçalvès, Thomas Stieglitz, Christine Vallet-Coulomb, Jérôme Labille, Vincent Marc, Angélique Poulain, and Philippe Dussouillez
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2023-239, https://doi.org/10.5194/hess-2023-239, 2024
Manuscript not accepted for further review
Short summary
Short summary
Understanding the relationship between rivers and alluvial aquifers is crucial, yet challenging. Through a combined approach of tracing and modeling in a French Rhône River site, we reveal significant insights. We quantify the impact of pumping on water flow and identify the primary water sources. Our findings aid sustainable water management in regions facing similar challenges, offering practical guidance for policymakers on groundwater use.
Gab Abramowitz, Anna Ukkola, Sanaa Hobeichi, Jon Cranko Page, Mathew Lipson, Martin De Kauwe, Sam Green, Claire Brenner, Jonathan Frame, Grey Nearing, Martyn Clark, Martin Best, Peter Anthoni, Gabriele Arduini, Souhail Boussetta, Silvia Caldararu, Kyeungwoo Cho, Matthias Cuntz, David Fairbairn, Craig Ferguson, Hyungjun Kim, Yeonjoo Kim, Jürgen Knauer, David Lawrence, Xiangzhong Luo, Sergey Malyshev, Tomoko Nitta, Jerome Ogee, Keith Oleson, Catherine Ottlé, Phillipe Peylin, Patricia de Rosnay, Heather Rumbold, Bob Su, Nicolas Vuichard, Anthony Walker, Xiaoni Wang-Faivre, Yunfei Wang, and Yijian Zeng
EGUsphere, https://doi.org/10.5194/egusphere-2023-3084, https://doi.org/10.5194/egusphere-2023-3084, 2024
Short summary
Short summary
This paper evaluates land models – computer based models that simulate ecosystem dynamics, the land carbon, water and energy cycles and the role of land in the climate system. It uses machine learning / AI approaches to show that despite the complexity of land models, they do not perform nearly as well as they could, given the amount of information they are provided with about the prediction problem.
Javier de la Casa, Adrià Barbeta, Asun Rodríguez-Uña, Lisa Wingate, Jérôme Ogée, and Teresa E. Gimeno
Hydrol. Earth Syst. Sci., 26, 4125–4146, https://doi.org/10.5194/hess-26-4125-2022, https://doi.org/10.5194/hess-26-4125-2022, 2022
Short summary
Short summary
Recently, studies have been reporting mismatches in the water isotopic composition of plants and soils. In this work, we reviewed worldwide isotopic composition data of field and laboratory studies to see if the mismatch is generalised, and we found it to be true. This contradicts theoretical expectations and may underlie an non-described phenomenon that should be forward investigated and implemented in ecohydrological models to avoid erroneous estimations of water sources used by vegetation.
Camille Abadie, Fabienne Maignan, Marine Remaud, Jérôme Ogée, J. Elliott Campbell, Mary E. Whelan, Florian Kitz, Felix M. Spielmann, Georg Wohlfahrt, Richard Wehr, Wu Sun, Nina Raoult, Ulli Seibt, Didier Hauglustaine, Sinikka T. Lennartz, Sauveur Belviso, David Montagne, and Philippe Peylin
Biogeosciences, 19, 2427–2463, https://doi.org/10.5194/bg-19-2427-2022, https://doi.org/10.5194/bg-19-2427-2022, 2022
Short summary
Short summary
A better constraint of the components of the carbonyl sulfide (COS) global budget is needed to exploit its potential as a proxy of gross primary productivity. In this study, we compare two representations of oxic soil COS fluxes, and we develop an approach to represent anoxic soil COS fluxes in a land surface model. We show the importance of atmospheric COS concentration variations on oxic soil COS fluxes and provide new estimates for oxic and anoxic soil contributions to the COS global budget.
Clément Outrequin, Anne Alexandre, Christine Vallet-Coulomb, Clément Piel, Sébastien Devidal, Amaelle Landais, Martine Couapel, Jean-Charles Mazur, Christophe Peugeot, Monique Pierre, Frédéric Prié, Jacques Roy, Corinne Sonzogni, and Claudia Voigt
Clim. Past, 17, 1881–1902, https://doi.org/10.5194/cp-17-1881-2021, https://doi.org/10.5194/cp-17-1881-2021, 2021
Short summary
Short summary
Continental atmospheric humidity is a key climate parameter poorly captured by global climate models. Model–data comparison approaches that are applicable beyond the instrumental period are essential to progress on this issue but face a lack of quantitative relative humidity proxies. Here, we calibrate the triple oxygen isotope composition of phytoliths as a new quantitative proxy of continental relative humidity suitable for past climate reconstructions.
Sam P. Jones, Aurore Kaisermann, Jérôme Ogée, Steven Wohl, Alexander W. Cheesman, Lucas A. Cernusak, and Lisa Wingate
SOIL, 7, 145–159, https://doi.org/10.5194/soil-7-145-2021, https://doi.org/10.5194/soil-7-145-2021, 2021
Short summary
Short summary
Understanding how the rate of oxygen isotope exchange between water and CO2 varies in soils is key for using the oxygen isotope composition of atmospheric CO2 as a tracer of biosphere CO2 fluxes at large scales. Across 44 diverse soils the rate of this exchange responded to pH, nitrate and microbial biomass, which are hypothesised to alter activity of the enzyme carbonic anhydrase in soils. Using these three soil traits, it is now possible to predict how this isotopic exchange varies spatially.
Claudia Voigt, Daniel Herwartz, Cristina Dorador, and Michael Staubwasser
Hydrol. Earth Syst. Sci., 25, 1211–1228, https://doi.org/10.5194/hess-25-1211-2021, https://doi.org/10.5194/hess-25-1211-2021, 2021
Short summary
Short summary
Evaporation trends in the stable isotope composition (18O/16O, 17O/16O, 2H/1H) of throughflow ponds in a hydrologically complex and seasonally dynamic lake system can be reliably predicted by the classic Craig–Gordon isotope evaporation model. We demonstrate that the novel 17O-excess parameter is capable of resolving different types of evaporation with and without recharge and of identifying mixing processes that cannot be resolved using the classic δ2H–δ18O system alone.
Anne Alexandre, Elizabeth Webb, Amaelle Landais, Clément Piel, Sébastien Devidal, Corinne Sonzogni, Martine Couapel, Jean-Charles Mazur, Monique Pierre, Frédéric Prié, Christine Vallet-Coulomb, Clément Outrequin, and Jacques Roy
Biogeosciences, 16, 4613–4625, https://doi.org/10.5194/bg-16-4613-2019, https://doi.org/10.5194/bg-16-4613-2019, 2019
Short summary
Short summary
This calibration study shows that despite isotope heterogeneity along grass leaves, the triple oxygen isotope composition of bulk leaf phytoliths can be estimated from the Craig and Gordon model, a mixing equation and a mean leaf water–phytolith fractionation exponent (lambda) of 0.521. The results strengthen the reliability of the 17O–excess of phytoliths to be used as a proxy of atmospheric relative humidity and open tracks for its use as an imprint of leaf water 17O–excess.
Chloé Poulin, Bruno Hamelin, Christine Vallet-Coulomb, Guinbe Amngar, Bichara Loukman, Jean-François Cretaux, Jean-Claude Doumnang, Abdallah Mahamat Nour, Guillemette Menot, Florence Sylvestre, and Pierre Deschamps
Hydrol. Earth Syst. Sci., 23, 1705–1724, https://doi.org/10.5194/hess-23-1705-2019, https://doi.org/10.5194/hess-23-1705-2019, 2019
Short summary
Short summary
This study investigates the water budget of two intertropical lake systems in the absence of long-term hydrological monitoring. By coupling dry season isotopic data with satellite imagery, we were able to provide quantitative constrains on the hydrological balance and show that these two lake systems can be considered miniature analogs of Lake Chad, making them important targets in the future setup of any large-scale program on the hydro-climatic evolution in the Sahel region.
Rosine Cartier, Florence Sylvestre, Christine Paillès, Corinne Sonzogni, Martine Couapel, Anne Alexandre, Jean-Charles Mazur, Elodie Brisset, Cécile Miramont, and Frédéric Guiter
Clim. Past, 15, 253–263, https://doi.org/10.5194/cp-15-253-2019, https://doi.org/10.5194/cp-15-253-2019, 2019
Short summary
Short summary
A major environmental change, 4200 years ago, was recorded in the lacustrine sediments of Lake Petit (Mediterranean Alps). The regime shift was described by a modification in erosion processes in the watershed and aquatic species in the lake. This study, based on the analysis of the lake water balance by using oxygen isotopes in diatoms, revealed that these environmental responses were due to a rapid change in precipitation regime, lasting ca. 500 years.
Anne-Cyrielle Genard-Zielinski, Christophe Boissard, Elena Ormeño, Juliette Lathière, Ilja M. Reiter, Henri Wortham, Jean-Philippe Orts, Brice Temime-Roussel, Bertrand Guenet, Svenja Bartsch, Thierry Gauquelin, and Catherine Fernandez
Biogeosciences, 15, 4711–4730, https://doi.org/10.5194/bg-15-4711-2018, https://doi.org/10.5194/bg-15-4711-2018, 2018
Short summary
Short summary
From seasonal in situ observations on how a Mediterranean ecosystem responds to drought, a specific isoprene emission (ER, emission rates) algorithm was developed, upon which 2100 projections (IPCC RCP2.6 and RCP8.5 scenarios) were made. Emission rates were found to be mainly sensitive to future temperature changes and poorly represented by current empirical emission models. Drought was found to aggravate thermal stress on emission rates.
Anne Alexandre, Amarelle Landais, Christine Vallet-Coulomb, Clément Piel, Sébastien Devidal, Sandrine Pauchet, Corinne Sonzogni, Martine Couapel, Marine Pasturel, Pauline Cornuault, Jingming Xin, Jean-Charles Mazur, Frédéric Prié, Ilhem Bentaleb, Elizabeth Webb, Françoise Chalié, and Jacques Roy
Biogeosciences, 15, 3223–3241, https://doi.org/10.5194/bg-15-3223-2018, https://doi.org/10.5194/bg-15-3223-2018, 2018
Short summary
Short summary
There is a lack of proxies suitable for reconstructing, in a quantitative way, past changes in continental atmospheric humidity, which is a key climate parameter. Here, we demonstrate through climate chamber and climate transect calibrations that the triple oxygen isotope composition of phytoliths offers a potential for reconstructing changes in relative humidity.
Camille Bouchez, Julio Goncalves, Pierre Deschamps, Christine Vallet-Coulomb, Bruno Hamelin, Jean-Claude Doumnang, and Florence Sylvestre
Hydrol. Earth Syst. Sci., 20, 1599–1619, https://doi.org/10.5194/hess-20-1599-2016, https://doi.org/10.5194/hess-20-1599-2016, 2016
Short summary
Short summary
Flows out of Lake Chad are constrained by a modeling of the hydrological, chemical, and isotopic budgets, based on a review of existing data along with new data. This innovative approach allows one to determine the proportions of evaporation, transpiration, and infiltration out of the lake while the two last flows are often neglected in semi-arid environments. Moreover, it allows to investigate the lake hydrological and chemical regulations under the large climatic changes in Sahel since 1950.
Anne Alexandre, Jérôme Balesdent, Patrick Cazevieille, Claire Chevassus-Rosset, Patrick Signoret, Jean-Charles Mazur, Araks Harutyunyan, Emmanuel Doelsch, Isabelle Basile-Doelsch, Hélène Miche, and Guaciara M. Santos
Biogeosciences, 13, 1693–1703, https://doi.org/10.5194/bg-13-1693-2016, https://doi.org/10.5194/bg-13-1693-2016, 2016
Short summary
Short summary
This 13C labeling experiment demonstrates that carbon can be absorbed by the roots, translocated in the plant, and ultimately fixed in organic compounds subject to occlusion in silica particles that form inside plant cells (phytoliths). Plausible forms of carbon absorbed, translocated, and fixed in phytoliths are assessed. Implications for our understanding of the C cycle at the plant-soil-atmosphere interface are discussed.
Paul E. Reyerson, Anne Alexandre, Araks Harutyunyan, Remi Corbineau, Hector A. Martinez De La Torre, Franz Badeck, Luigi Cattivelli, and Guaciara M. Santos
Biogeosciences, 13, 1269–1286, https://doi.org/10.5194/bg-13-1269-2016, https://doi.org/10.5194/bg-13-1269-2016, 2016
Short summary
Short summary
We characterize the origin of carbon (C) in phytoliths (biosilica of higher plants) by a multi-isotope approach. We show that phytoliths occlude soil organic C adsorbed through the roots, making them unsuitable for paleo-proxy studies, 14C dating or atmospheric CO2 sequestration. Our findings are in parallel with recent soil paradigm shifts showing that soil microbes access old C and therefore call for further investigations on the role of old C in root–plant interactions and biomineralization.
H. Delattre, C. Vallet-Coulomb, and C. Sonzogni
Atmos. Chem. Phys., 15, 10167–10181, https://doi.org/10.5194/acp-15-10167-2015, https://doi.org/10.5194/acp-15-10167-2015, 2015
Short summary
Short summary
Based on summer measurements of δ18O and δD in the atmospheric vapour of a Mediterranean coastal wetland exposed to high evaporation, this paper explores the main drivers of isotopic signal variability. After having classified the data according to the main regional air mass trajectories, average diurnal cycles are discussed with regards to the contribution of local evaporation to the ground level atmospheric vapour.
A. Alexandre, I. Basile-Doelsch, T. Delhaye, D. Borshneck, J. C. Mazur, P. Reyerson, and G. M. Santos
Biogeosciences, 12, 863–873, https://doi.org/10.5194/bg-12-863-2015, https://doi.org/10.5194/bg-12-863-2015, 2015
Short summary
Short summary
Phytoliths contain occluded organic compounds called phytC. The nature and location of phytC in biogenic silica structures is poorly understood. Here, we reconstructed the 3-D structure of phytoliths using 3-D Xray microscopy. We further evidenced a pool of phytC, continuously distributed in the silica structure, using nanoscale secondary ion mass spectrometry (NanoSIMS). Our findings allowed the re-evaluation of previous suggestions regarding phytC quantification and environmental meaning.
M. C. Matteuzzo, A. Alexandre, A. F. D. C. Varajão, C. Volkmer-Ribeiro, A. C. S. Almeida, C. A. C. Varajão, C. Vallet-Coulomb, C. Sonzogni, and H. Miche
Biogeosciences Discuss., https://doi.org/10.5194/bgd-10-12887-2013, https://doi.org/10.5194/bgd-10-12887-2013, 2013
Revised manuscript not accepted
Related subject area
Paleobiogeoscience: Proxy use, Development & Validation
A long-term drought reconstruction based on oxygen isotope tree ring data
Disentangling influences of climate variability and lake-system evolution on climate proxies derived from isoprenoid and branched glycerol dialkyl glycerol tetraethers (GDGTs): the 250 kyr Lake Chala record
Electron backscatter diffraction analysis unveils foraminiferal calcite microstructure and processes of diagenetic alteration
Quantifying the δ15N trophic offset in a cold-water scleractinian coral (CWC): implications for the CWC diet and coral δ15N as a marine N cycle proxy
Stable oxygen isotopes of crocodilian tooth enamel allow tracking Plio-Pleistocene evolution of freshwater environments and climate in the Shungura Formation (Turkana Depression, Ethiopia)
Reviews and syntheses: Review of proxies for low-oxygen paleoceanographic reconstructions
Charcoal morphologies and morphometrics of a Eurasian grass-dominated system for robust interpretation of past fuel and fire type
Single-species dinoflagellate cyst carbon isotope fractionation in core-top sediments: environmental controls, CO2 dependency and proxy potential
Past fire dynamics inferred from polycyclic aromatic hydrocarbons and monosaccharide anhydrides in a stalagmite from the archaeological site of Mayapan, Mexico
Biomarker characterization of the North Water Polynya, Baffin Bay: implications for local sea ice and temperature proxies
Technical note: No impact of alkenone extraction on foraminiferal stable isotope, trace element and boron isotope geochemistry
Deep-sea stylasterid δ18O and δ13C maps inform sampling scheme for paleotemperature reconstructions
Experimental burial diagenesis of aragonitic biocarbonates: from organic matter loss to abiogenic calcite formation
A modern snapshot of the isotopic composition of lacustrine biogenic carbonates – records of seasonal water temperature variability
Performance of temperature and productivity proxies based on long-chain alkane-1, mid-chain diols at test: a 5-year sediment trap record from the Mauritanian upwelling
Validation of a coupled δ2Hn-alkane–δ18Osugar paleohygrometer approach based on a climate chamber experiment
Experimental production of charcoal morphologies to discriminate fuel source and fire type: an example from Siberian taiga
Toward a global calibration for quantifying past oxygenation in oxygen minimum zones using benthic Foraminifera
Calibration of Mg ∕ Ca and Sr ∕ Ca in coastal marine ostracods as a proxy for temperature
Technical note: Accelerate coccolith size separation via repeated centrifugation
Mg∕Ca, Sr∕Ca and stable isotopes from the planktonic foraminifera T. sacculifer: testing a multi-proxy approach for inferring paleotemperature and paleosalinity
Chemical destaining and the delta correction for blue intensity measurements of stained lake subfossil trees
Modern calibration of Poa flabellata (tussac grass) as a new paleoclimate proxy in the South Atlantic
Seawater pH reconstruction using boron isotopes in multiple planktonic foraminifera species with different depth habitats and their potential to constrain pH and pCO2 gradients
Bottom-water deoxygenation at the Peruvian margin during the last deglaciation recorded by benthic foraminifera
The pH dependency of the boron isotopic composition of diatom opal (Thalassiosira weissflogii)
Benthic foraminifera as tracers of brine production in the Storfjorden “sea ice factory”
Evaluation of bacterial glycerol dialkyl glycerol tetraether and 2H–18O biomarker proxies along a central European topsoil transect
Leaf wax n-alkane patterns and compound-specific δ13C of plants and topsoils from semi-arid and arid Mongolia
Organic-carbon-rich sediments: benthic foraminifera as bio-indicators of depositional environments
Strong correspondence between nitrogen isotope composition of foliage and chlorin across a rainfall gradient: implications for paleo-reconstruction of the nitrogen cycle
Environmental and biological controls on Na∕Ca ratios in scleractinian cold-water corals
Depth habitat of the planktonic foraminifera Neogloboquadrina pachyderma in the northern high latitudes explained by sea-ice and chlorophyll concentrations
Temporal variability in foraminiferal morphology and geochemistry at the West Antarctic Peninsula: a sediment trap study
Seasonality of archaeal lipid flux and GDGT-based thermometry in sinking particles of high-latitude oceans: Fram Strait (79° N) and Antarctic Polar Front (50° S)
Long-chain diols in settling particles in tropical oceans: insights into sources, seasonality and proxies
Multi-trace-element sea surface temperature coral reconstruction for the southern Mozambique Channel reveals teleconnections with the tropical Atlantic
Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth
Mg ∕ Ca and δ18O in living planktic foraminifers from the Caribbean, Gulf of Mexico and Florida Straits
Manganese incorporation in living (stained) benthic foraminiferal shells: a bathymetric and in-sediment study in the Gulf of Lions (NW Mediterranean)
Effects of light and temperature on Mg uptake, growth, and calcification in the proxy climate archive Clathromorphum compactum
A systematic look at chromium isotopes in modern shells – implications for paleo-environmental reconstructions
Reviews and syntheses: Revisiting the boron systematics of aragonite and their application to coral calcification
Physico-chemical and biological factors influencing dinoflagellate cyst production in the Cariaco Basin
Effects of alkalinity and salinity at low and high light intensity on hydrogen isotope fractionation of long-chain alkenones produced by Emiliania huxleyi
Interplay of community dynamics, temperature, and productivity on the hydrogen isotope signatures of lipid biomarkers
Benthic foraminiferal Mn / Ca ratios reflect microhabitat preferences
The effects of environment on Arctica islandica shell formation and architecture
Diatoms as a paleoproductivity proxy in the NW Iberian coastal upwelling system (NE Atlantic)
Factors controlling the depth habitat of planktonic foraminifera in the subtropical eastern North Atlantic
Viorica Nagavciuc, Gerhard Helle, Maria Rădoane, Cătălin-Constantin Roibu, Mihai-Gabriel Cotos, and Monica Ionita
EGUsphere, https://doi.org/10.5194/egusphere-2024-2144, https://doi.org/10.5194/egusphere-2024-2144, 2024
Short summary
Short summary
We reconstructed drought conditions for the past 200 years using δ18O in oak tree ring cellulose from Romania, revealing periods of both extreme wetness (e.g., 1905–1915) and dryness (e.g., 1818–1835). The most severe droughts occurred in the 19th and 21st centuries. The study suggests a connection between drought patterns and large-scale atmospheric circulation. This research highlights the potential of tree rings to improve our understanding of long-term climate variability in Europe.
Allix J. Baxter, Francien Peterse, Dirk Verschuren, Aihemaiti Maitituerdi, Nicolas Waldmann, and Jaap S. Sinninghe Damsté
Biogeosciences, 21, 2877–2908, https://doi.org/10.5194/bg-21-2877-2024, https://doi.org/10.5194/bg-21-2877-2024, 2024
Short summary
Short summary
This study investigates the impact of long-term lake-system evolution on the climate signal recorded by glycerol dialkyl glycerol tetraethers (GDGTs), a popular biomarker in paleoclimate research. It compares downcore changes in GDGTs in the 250 000 year sediment sequence of Lake Chala (Kenya/Tanzania) to independent data for lake mixing and water-column chemistry. These factors influence the GDGT proxies in the earliest depositional phases (before ~180 ka), confounding the climate signal.
Frances A. Procter, Sandra Piazolo, Eleanor H. John, Richard Walshaw, Paul N. Pearson, Caroline H. Lear, and Tracy Aze
Biogeosciences, 21, 1213–1233, https://doi.org/10.5194/bg-21-1213-2024, https://doi.org/10.5194/bg-21-1213-2024, 2024
Short summary
Short summary
This study uses novel techniques to look at the microstructure of planktonic foraminifera (single-celled marine organisms) fossils, to further our understanding of how they form their hard exterior shells and how the microstructure and chemistry of these shells can change as a result of processes that occur after deposition on the seafloor. Understanding these processes is of critical importance for using planktonic foraminifera for robust climate and environmental reconstructions of the past.
Josie L. Mottram, Anne M. Gothmann, Maria G. Prokopenko, Austin Cordova, Veronica Rollinson, Katie Dobkowski, and Julie Granger
Biogeosciences, 21, 1071–1091, https://doi.org/10.5194/bg-21-1071-2024, https://doi.org/10.5194/bg-21-1071-2024, 2024
Short summary
Short summary
Knowledge of ancient ocean N cycling can help illuminate past climate change. Using field and lab studies, this work ground-truths a promising proxy for marine N cycling, the N isotope composition of cold-water coral (CWC) skeletons. Our results estimate N turnover in CWC tissue; quantify the isotope effects between CWC tissue, diet, and skeleton; and suggest that CWCs possibly feed mainly on metazoan zooplankton, suggesting that the marine N proxy may be sensitive to the food web structure.
Axelle Gardin, Emmanuelle Pucéat, Géraldine Garcia, Jean-Renaud Boisserie, Adélaïde Euriat, Michael M. Joachimski, Alexis Nutz, Mathieu Schuster, and Olga Otero
Biogeosciences, 21, 437–454, https://doi.org/10.5194/bg-21-437-2024, https://doi.org/10.5194/bg-21-437-2024, 2024
Short summary
Short summary
We introduce a novel approach using stable oxygen isotopes from crocodilian fossil teeth to unravel palaeohydrological changes in past continental contexts. Applying it to the Plio-Pleistocene Ethiopian Shungura Formation, we found a significant increase in δ18O in the last 3 million years, likely due to monsoonal shifts and reduced rainfall, and that the local diversity of waterbodies (lakes, rivers, ponds) became restricted.
Babette Hoogakker, Catherine Davis, Yi Wang, Stepanie Kusch, Katrina Nilsson-Kerr, Dalton Hardisty, Allison Jacobel, Dharma Reyes Macaya, Nicolaas Glock, Sha Ni, Julio Sepúlveda, Abby Ren, Alexandra Auderset, Anya Hess, Katrina Meissner, Jorge Cardich, Robert Anderson, Christine Barras, Chandranath Basak, Harold Bradbury, Inda Brinkmann, Alexis Castillo, Madelyn Cook, Kassandra Costa, Constance Choquel, Paula Diz, Jonas Donnenfield, Felix Elling, Zeynep Erdem, Helena Filipsson, Sebastian Garrido, Julia Gottschalk, Anjaly Govindankutty Menon, Jeroen Groeneveld, Christian Hallman, Ingrid Hendy, Rick Hennekam, Wanyi Lu, Jean Lynch-Stieglitz, Lelia Matos, Alfredo Martínez-García, Giulia Molina, Práxedes Muñoz, Simone Moretti, Jennifer Morford, Sophie Nuber, Svetlana Radionovskaya, Morgan Raven, Christopher Somes, Anja Studer, Kazuyo Tachikawa, Raúl Tapia, Martin Tetard, Tyler Vollmer, Shuzhuang Wu, Yan Zhang, Xin-Yuan Zheng, and Yuxin Zhou
EGUsphere, https://doi.org/10.5194/egusphere-2023-2981, https://doi.org/10.5194/egusphere-2023-2981, 2024
Short summary
Short summary
Paleo-oxygen proxies can extend current records, bound pre-anthropogenic baselines, provide datasets necessary to test climate models under different boundary conditions, and ultimately understand how ocean oxygenation responds on longer timescales. Here we summarize current proxies used for the reconstruction of Cenozoic seawater oxygen levels. This includes an overview of the proxy's history, how it works, resources required, limitations, and future recommendations.
Angelica Feurdean, Richard S. Vachula, Diana Hanganu, Astrid Stobbe, and Maren Gumnior
Biogeosciences, 20, 5069–5085, https://doi.org/10.5194/bg-20-5069-2023, https://doi.org/10.5194/bg-20-5069-2023, 2023
Short summary
Short summary
This paper presents novel results of laboratory-produced charcoal forms from various grass, forb and shrub taxa from the Eurasian steppe to facilitate more robust interpretations of fuel sources and fire types in grassland-dominated ecosystems. Advancements in identifying fuel sources and changes in fire types make charcoal analysis relevant to studies of plant evolution and fire management.
Joost Frieling, Linda van Roij, Iris Kleij, Gert-Jan Reichart, and Appy Sluijs
Biogeosciences, 20, 4651–4668, https://doi.org/10.5194/bg-20-4651-2023, https://doi.org/10.5194/bg-20-4651-2023, 2023
Short summary
Short summary
We present a first species-specific evaluation of marine core-top dinoflagellate cyst carbon isotope fractionation (εp) to assess natural pCO2 dependency on εp and explore its geological deep-time paleo-pCO2 proxy potential. We find that εp differs between genera and species and that in Operculodinium centrocarpum, εp is controlled by pCO2 and nutrients. Our results highlight the added value of δ13C analyses of individual micrometer-scale sedimentary organic carbon particles.
Julia Homann, Niklas Karbach, Stacy A. Carolin, Daniel H. James, David Hodell, Sebastian F. M. Breitenbach, Ola Kwiecien, Mark Brenner, Carlos Peraza Lope, and Thorsten Hoffmann
Biogeosciences, 20, 3249–3260, https://doi.org/10.5194/bg-20-3249-2023, https://doi.org/10.5194/bg-20-3249-2023, 2023
Short summary
Short summary
Cave stalagmites contain substances that can be used to reconstruct past changes in local and regional environmental conditions. We used two classes of biomarkers (polycyclic aromatic hydrocarbons and monosaccharide anhydrides) to detect the presence of fire and to also explore changes in fire regime (e.g. fire frequency, intensity, and fuel source). We tested our new method on a stalagmite from Mayapan, a large Maya city on the Yucatán Peninsula.
David J. Harning, Brooke Holman, Lineke Woelders, Anne E. Jennings, and Julio Sepúlveda
Biogeosciences, 20, 229–249, https://doi.org/10.5194/bg-20-229-2023, https://doi.org/10.5194/bg-20-229-2023, 2023
Short summary
Short summary
In order to better reconstruct the geologic history of the North Water Polynya, we provide modern validations and calibrations of lipid biomarker proxies in Baffin Bay. We find that sterols, rather than HBIs, most accurately capture the current extent of the North Water Polynya and will be a valuable tool to reconstruct its past presence or absence. Our local temperature calibrations for GDGTs and OH-GDGTs reduce the uncertainty present in global temperature calibrations.
Jessica G. M. Crumpton-Banks, Thomas Tanner, Ivan Hernández Almeida, James W. B. Rae, and Heather Stoll
Biogeosciences, 19, 5633–5644, https://doi.org/10.5194/bg-19-5633-2022, https://doi.org/10.5194/bg-19-5633-2022, 2022
Short summary
Short summary
Past ocean carbon is reconstructed using proxies, but it is unknown whether preparing ocean sediment for one proxy might damage the data given by another. We have tested whether the extraction of an organic proxy archive from sediment samples impacts the geochemistry of tiny shells also within the sediment. We find no difference in shell geochemistry between samples which come from treated and untreated sediment. This will help us to maximize scientific return from valuable sediment samples.
Theresa M. King and Brad E. Rosenheim
Biogeosciences Discuss., https://doi.org/10.5194/bg-2022-180, https://doi.org/10.5194/bg-2022-180, 2022
Revised manuscript accepted for BG
Short summary
Short summary
Corals can record ocean properties such as temperature in their skeletons. These records are useful for where and when we have no instrumental record like in the distant past. However, coral growth must be understood to interpret these records. Here, we analyze slices of a branching deep sea coral from Antarctica to determine how to best sample these corals for past climate work. We recommend sampling from the innermost portion of coral skeleton for accurate temperature reconstructions.
Pablo Forjanes, María Simonet Roda, Martina Greiner, Erika Griesshaber, Nelson A. Lagos, Sabino Veintemillas-Verdaguer, José Manuel Astilleros, Lurdes Fernández-Díaz, and Wolfgang W. Schmahl
Biogeosciences, 19, 3791–3823, https://doi.org/10.5194/bg-19-3791-2022, https://doi.org/10.5194/bg-19-3791-2022, 2022
Short summary
Short summary
Aragonitic skeletons are employed to decipher past climate dynamics and environmental change. Unfortunately, the information that these skeletons keep can be destroyed during diagenesis. In this work, we study the first changes undergone by aragonitic skeletons upon hydrothermal alteration. We observe that major changes occur from the very beginning of the alteration, even without mineralogical changes. These results have major implications for the use of these archives to understand the past.
Inga Labuhn, Franziska Tell, Ulrich von Grafenstein, Dan Hammarlund, Henning Kuhnert, and Bénédicte Minster
Biogeosciences, 19, 2759–2777, https://doi.org/10.5194/bg-19-2759-2022, https://doi.org/10.5194/bg-19-2759-2022, 2022
Short summary
Short summary
This study presents the isotopic composition of recent biogenic carbonates from several lacustrine species which calcify during different times of the year. The authors demonstrate that when biological offsets are corrected, the dominant cause of differences between species is the seasonal variation in temperature-dependent fractionation of oxygen isotopes. Consequently, such carbonates from lake sediments can provide proxy records of seasonal water temperature changes in the past.
Gerard J. M. Versteegh, Karin A. F. Zonneveld, Jens Hefter, Oscar E. Romero, Gerhard Fischer, and Gesine Mollenhauer
Biogeosciences, 19, 1587–1610, https://doi.org/10.5194/bg-19-1587-2022, https://doi.org/10.5194/bg-19-1587-2022, 2022
Short summary
Short summary
A 5-year record of long-chain mid-chain diol export flux and composition is presented with a 1- to 3-week resolution sediment trap CBeu (in the NW African upwelling). All environmental parameters as well as the diol composition are dominated by the seasonal cycle, albeit with different phase relations for temperature and upwelling. Most diol-based proxies are dominated by upwelling. The long-chain diol index reflects temperatures of the oligotrophic summer sea surface.
Johannes Hepp, Christoph Mayr, Kazimierz Rozanski, Imke Kathrin Schäfer, Mario Tuthorn, Bruno Glaser, Dieter Juchelka, Willibald Stichler, Roland Zech, and Michael Zech
Biogeosciences, 18, 5363–5380, https://doi.org/10.5194/bg-18-5363-2021, https://doi.org/10.5194/bg-18-5363-2021, 2021
Short summary
Short summary
Deriving more quantitative climate information like relative air humidity is one of the key challenges in paleostudies. Often only qualitative reconstructions can be done when single-biomarker-isotope data are derived from a climate archive. However, the coupling of hemicellulose-derived sugar with leaf-wax-derived n-alkane isotope results has the potential to overcome this limitation and allow a quantitative relative air humidity reconstruction.
Angelica Feurdean
Biogeosciences, 18, 3805–3821, https://doi.org/10.5194/bg-18-3805-2021, https://doi.org/10.5194/bg-18-3805-2021, 2021
Short summary
Short summary
This study characterized the diversity of laboratory-produced charcoal morphological features of various fuel types from Siberia at different temperatures. The results obtained improve the attribution of charcoal particles to fuel types and fire characteristics. This work also provides recommendations for the application of this information to refine the past wildfire history.
Martin Tetard, Laetitia Licari, Ekaterina Ovsepyan, Kazuyo Tachikawa, and Luc Beaufort
Biogeosciences, 18, 2827–2841, https://doi.org/10.5194/bg-18-2827-2021, https://doi.org/10.5194/bg-18-2827-2021, 2021
Short summary
Short summary
Oxygen minimum zones are oceanic regions almost devoid of dissolved oxygen and are currently expanding due to global warming. Investigation of their past behaviour will allow better understanding of these areas and better prediction of their future evolution. A new method to estimate past [O2] was developed based on morphometric measurements of benthic foraminifera. This method and two other approaches based on foraminifera assemblages and porosity were calibrated using 45 core tops worldwide.
Maximiliano Rodríguez and Christelle Not
Biogeosciences, 18, 1987–2001, https://doi.org/10.5194/bg-18-1987-2021, https://doi.org/10.5194/bg-18-1987-2021, 2021
Short summary
Short summary
Mg/Ca in calcium carbonate shells of marine organisms such as foraminifera and ostracods has been used as a proxy to reconstruct water temperature. Here we provide new Mg/Ca–temperature calibrations for two shallow marine species of ostracods. We show that the water temperature in spring produces the best calibrations, which suggests the potential use of ostracod shells to reconstruct this parameter at a seasonal scale.
Hongrui Zhang, Chuanlian Liu, Luz María Mejía, and Heather Stoll
Biogeosciences, 18, 1909–1916, https://doi.org/10.5194/bg-18-1909-2021, https://doi.org/10.5194/bg-18-1909-2021, 2021
Delphine Dissard, Gert Jan Reichart, Christophe Menkes, Morgan Mangeas, Stephan Frickenhaus, and Jelle Bijma
Biogeosciences, 18, 423–439, https://doi.org/10.5194/bg-18-423-2021, https://doi.org/10.5194/bg-18-423-2021, 2021
Short summary
Short summary
Results from a data set acquired from living foraminifera T. sacculifer collected from surface waters are presented, allowing us to establish a new Mg/Ca–Sr/Ca–temperature equation improving temperature reconstructions. When combining equations, δ18Ow can be reconstructed with a precision of ± 0.5 ‰, while successive reconstructions involving Mg/Ca and δ18Oc preclude salinity reconstruction with a precision better than ± 1.69. A new direct linear fit to reconstruct salinity could be established.
Feng Wang, Dominique Arseneault, Étienne Boucher, Shulong Yu, Steeven Ouellet, Gwenaëlle Chaillou, Ann Delwaide, and Lily Wang
Biogeosciences, 17, 4559–4570, https://doi.org/10.5194/bg-17-4559-2020, https://doi.org/10.5194/bg-17-4559-2020, 2020
Short summary
Short summary
Wood stain is challenging the use of the blue intensity technique for dendroclimatic reconstructions. Using stained subfossil trees from eastern Canadian lakes, we compared chemical destaining approaches with the
delta bluemathematical correction of blue intensity data. Although no chemical treatment was completely efficient, the delta blue method is unaffected by the staining problem and thus is promising for climate reconstructions based on lake subfossil material.
Dulcinea V. Groff, David G. Williams, and Jacquelyn L. Gill
Biogeosciences, 17, 4545–4557, https://doi.org/10.5194/bg-17-4545-2020, https://doi.org/10.5194/bg-17-4545-2020, 2020
Short summary
Short summary
Tussock grasses that grow along coastlines of the Falkland Islands are slow to decay and build up thick peat layers over thousands of years. Grass fragments found in ancient peat can be used to reconstruct past climate because grasses can preserve a record of growing conditions in their leaves. We found that modern living tussock grasses in the Falkland Islands reliably record temperature and humidity in their leaves, and the peat they form can be used to understand past climate change.
Maxence Guillermic, Sambuddha Misra, Robert Eagle, Alexandra Villa, Fengming Chang, and Aradhna Tripati
Biogeosciences, 17, 3487–3510, https://doi.org/10.5194/bg-17-3487-2020, https://doi.org/10.5194/bg-17-3487-2020, 2020
Short summary
Short summary
Boron isotope ratios (δ11B) of foraminifera are a promising proxy for seawater pH and can be used to constrain pCO2. In this study, we derived calibrations for new foraminiferal taxa which extend the application of the boron isotope proxy. We discuss the origin of different δ11B signatures in species and also discuss the potential of using multispecies δ11B analyses to constrain vertical pH and pCO2 gradients in ancient water columns to shed light on biogeochemical carbon cycling in the past.
Zeynep Erdem, Joachim Schönfeld, Anthony E. Rathburn, Maria-Elena Pérez, Jorge Cardich, and Nicolaas Glock
Biogeosciences, 17, 3165–3182, https://doi.org/10.5194/bg-17-3165-2020, https://doi.org/10.5194/bg-17-3165-2020, 2020
Short summary
Short summary
Recent observations from today’s oceans revealed that oxygen concentrations are decreasing, and oxygen minimum zones are expanding together with current climate change. With the aim of understanding past climatic events and their relationship with oxygen content, we looked at the fossils, called benthic foraminifera, preserved in the sediment archives from the Peruvian margin and quantified the bottom-water oxygen content for the last 22 000 years.
Hannah K. Donald, Gavin L. Foster, Nico Fröhberg, George E. A. Swann, Alex J. Poulton, C. Mark Moore, and Matthew P. Humphreys
Biogeosciences, 17, 2825–2837, https://doi.org/10.5194/bg-17-2825-2020, https://doi.org/10.5194/bg-17-2825-2020, 2020
Short summary
Short summary
The boron isotope pH proxy is increasingly being used to reconstruct ocean pH in the past. Here we detail a novel analytical methodology for measuring the boron isotopic composition (δ11B) of diatom opal and apply this to the study of the diatom Thalassiosira weissflogii grown in culture over a range of pH. To our knowledge this is the first study of its kind and provides unique insights into the way in which diatoms incorporate boron and their potential as archives of palaeoclimate records.
Eleonora Fossile, Maria Pia Nardelli, Arbia Jouini, Bruno Lansard, Antonio Pusceddu, Davide Moccia, Elisabeth Michel, Olivier Péron, Hélène Howa, and Meryem Mojtahid
Biogeosciences, 17, 1933–1953, https://doi.org/10.5194/bg-17-1933-2020, https://doi.org/10.5194/bg-17-1933-2020, 2020
Short summary
Short summary
This study focuses on benthic foraminiferal distribution in an Arctic fjord characterised by continuous sea ice production during winter and the consequent cascading of salty and corrosive waters (brine) to the seabed. The inner fjord is dominated by calcareous species (C). In the central deep basins, where brines are persistent, calcareous foraminifera are dissolved and agglutinated (A) dominate. The high A/C ratio is suggested as a proxy for brine persistence and sea ice production.
Johannes Hepp, Imke Kathrin Schäfer, Verena Lanny, Jörg Franke, Marcel Bliedtner, Kazimierz Rozanski, Bruno Glaser, Michael Zech, Timothy Ian Eglinton, and Roland Zech
Biogeosciences, 17, 741–756, https://doi.org/10.5194/bg-17-741-2020, https://doi.org/10.5194/bg-17-741-2020, 2020
Julian Struck, Marcel Bliedtner, Paul Strobel, Jens Schumacher, Enkhtuya Bazarradnaa, and Roland Zech
Biogeosciences, 17, 567–580, https://doi.org/10.5194/bg-17-567-2020, https://doi.org/10.5194/bg-17-567-2020, 2020
Short summary
Short summary
We present leaf wax n-alkanes and their compound-specific (CS) δ13C isotopes from semi-arid and/or arid Mongolia to test their potential for paleoenvironmental reconstructions. Plants and topsoils were analysed and checked for climatic control. Chain-length variations are distinct between grasses and Caragana, which are not biased by climate. However CS δ13C is strongly correlated to climate, so n-alkanes and their CS δ13C show great potential for paleoenvironmental reconstruction in Mongolia.
Elena Lo Giudice Cappelli, Jessica Louise Clarke, Craig Smeaton, Keith Davidson, and William Edward Newns Austin
Biogeosciences, 16, 4183–4199, https://doi.org/10.5194/bg-16-4183-2019, https://doi.org/10.5194/bg-16-4183-2019, 2019
Short summary
Short summary
Fjords are known sinks of organic carbon (OC); however, little is known about the long-term fate of the OC stored in these sediments. The reason for this knowledge gap is the post-depositional degradation of OC. This study uses benthic foraminifera (microorganisms with calcite shells) to discriminate between post-depositional OC degradation and actual OC burial and accumulation in fjordic sediments, as foraminifera would only preserve the latter information in their assemblage composition.
Sara K. E. Goulden, Naohiko Ohkouchi, Katherine H. Freeman, Yoshito Chikaraishi, Nanako O. Ogawa, Hisami Suga, Oliver Chadwick, and Benjamin Z. Houlton
Biogeosciences, 16, 3869–3882, https://doi.org/10.5194/bg-16-3869-2019, https://doi.org/10.5194/bg-16-3869-2019, 2019
Short summary
Short summary
We investigate whether soil organic compounds preserve information about nitrogen availability to plants. We isolate chlorophyll degradation products in leaves, litter, and soil and explore possible species and climate effects on preservation and interpretation. We find that compound-specific nitrogen isotope measurements in soil have potential as a new tool to reconstruct changes in nitrogen cycling on a landscape over time, avoiding issues that have limited other proxies.
Nicolai Schleinkofer, Jacek Raddatz, André Freiwald, David Evans, Lydia Beuck, Andres Rüggeberg, and Volker Liebetrau
Biogeosciences, 16, 3565–3582, https://doi.org/10.5194/bg-16-3565-2019, https://doi.org/10.5194/bg-16-3565-2019, 2019
Short summary
Short summary
In this study we tried to correlate Na / Ca ratios from cold-water corals with environmental parameters such as salinity, temperature and pH. We do not observe a correlation between Na / Ca ratios and seawater salinity, but we do observe a strong correlation with temperature. Na / Ca data from warm-water corals (Porites spp.) and bivalves (Mytilus edulis) support this correlation, indicating that similar controls on the incorporation of sodium exist in these aragonitic organisms.
Mattia Greco, Lukas Jonkers, Kerstin Kretschmer, Jelle Bijma, and Michal Kucera
Biogeosciences, 16, 3425–3437, https://doi.org/10.5194/bg-16-3425-2019, https://doi.org/10.5194/bg-16-3425-2019, 2019
Short summary
Short summary
To be able to interpret the paleoecological signal contained in N. pachyderma's shells, its habitat depth must be known. Our investigation on 104 density profiles of this species from the Arctic and North Atlantic shows that specimens reside closer to the surface when sea-ice and/or surface chlorophyll concentrations are high. This is in contrast with previous investigations that pointed at the position of the deep chlorophyll maximum as the main driver of N. pachyderma vertical distribution.
Anna Mikis, Katharine R. Hendry, Jennifer Pike, Daniela N. Schmidt, Kirsty M. Edgar, Victoria Peck, Frank J. C. Peeters, Melanie J. Leng, Michael P. Meredith, Chloe L. C. Jones, Sharon Stammerjohn, and Hugh Ducklow
Biogeosciences, 16, 3267–3282, https://doi.org/10.5194/bg-16-3267-2019, https://doi.org/10.5194/bg-16-3267-2019, 2019
Short summary
Short summary
Antarctic marine calcifying organisms are threatened by regional climate change and ocean acidification. Future projections of regional carbonate production are challenging due to the lack of historical data combined with complex climate variability. We present a 6-year record of flux, morphology and geochemistry of an Antarctic planktonic foraminifera, which shows that their growth is most sensitive to sea ice dynamics and is linked with the El Niño–Southern Oscillation.
Eunmi Park, Jens Hefter, Gerhard Fischer, Morten Hvitfeldt Iversen, Simon Ramondenc, Eva-Maria Nöthig, and Gesine Mollenhauer
Biogeosciences, 16, 2247–2268, https://doi.org/10.5194/bg-16-2247-2019, https://doi.org/10.5194/bg-16-2247-2019, 2019
Short summary
Short summary
We analyzed GDGT-based proxy temperatures in the polar oceans. In the eastern Fram Strait (79° N), the nutrient distribution may determine the depth habit of Thaumarchaeota and thus the proxy temperature. In the Antarctic Polar Front (50° S), the contribution of Euryarchaeota or the nonlinear correlation between the proxy values and temperatures may cause the warm biases of the proxy temperatures relative to SSTs.
Marijke W. de Bar, Jenny E. Ullgren, Robert C. Thunnell, Stuart G. Wakeham, Geert-Jan A. Brummer, Jan-Berend W. Stuut, Jaap S. Sinninghe Damsté, and Stefan Schouten
Biogeosciences, 16, 1705–1727, https://doi.org/10.5194/bg-16-1705-2019, https://doi.org/10.5194/bg-16-1705-2019, 2019
Short summary
Short summary
We analyzed sediment traps from the Cariaco Basin, the tropical Atlantic and the Mozambique Channel to evaluate seasonal imprints in the concentrations and fluxes of long-chain diols (LDIs), in addition to the long-chain diol index proxy (sea surface temperature proxy) and the diol index (upwelling indicator). Despite significant degradation, LDI-derived temperatures were very similar for the sediment traps and seafloor sediments, and corresponded to annual mean sea surface temperatures.
Jens Zinke, Juan P. D'Olivo, Christoph J. Gey, Malcolm T. McCulloch, J. Henrich Bruggemann, Janice M. Lough, and Mireille M. M. Guillaume
Biogeosciences, 16, 695–712, https://doi.org/10.5194/bg-16-695-2019, https://doi.org/10.5194/bg-16-695-2019, 2019
Short summary
Short summary
Here we report seasonally resolved sea surface temperature (SST) reconstructions for the southern Mozambique Channel in the SW Indian Ocean, a region located along the thermohaline ocean surface circulation route, based on multi-trace-element temperature proxy records preserved in two Porites sp. coral cores for the past 42 years. Particularly, we show the suitability of both separate and combined Sr / Ca and Li / Mg proxies for improved multielement SST reconstructions.
Hilde Pracht, Brett Metcalfe, and Frank J. C. Peeters
Biogeosciences, 16, 643–661, https://doi.org/10.5194/bg-16-643-2019, https://doi.org/10.5194/bg-16-643-2019, 2019
Short summary
Short summary
In palaeoceanography the shells of single-celled foraminifera are routinely used as proxies to reconstruct the temperature, salinity and circulation of the ocean in the past. Traditionally a number of specimens were pooled for a single stable isotope measurement; however, technical advances now mean that a single shell or chamber of a shell can be measured individually. Three different hypotheses regarding foraminiferal biology and ecology were tested using this approach.
Anna Jentzen, Dirk Nürnberg, Ed C. Hathorne, and Joachim Schönfeld
Biogeosciences, 15, 7077–7095, https://doi.org/10.5194/bg-15-7077-2018, https://doi.org/10.5194/bg-15-7077-2018, 2018
Shauna Ní Fhlaithearta, Christophe Fontanier, Frans Jorissen, Aurélia Mouret, Adriana Dueñas-Bohórquez, Pierre Anschutz, Mattias B. Fricker, Detlef Günther, Gert J. de Lange, and Gert-Jan Reichart
Biogeosciences, 15, 6315–6328, https://doi.org/10.5194/bg-15-6315-2018, https://doi.org/10.5194/bg-15-6315-2018, 2018
Short summary
Short summary
This study looks at how foraminifera interact with their geochemical environment in the seabed. We focus on the incorporation of the trace metal manganese (Mn), with the aim of developing a tool to reconstruct past pore water profiles. Manganese concentrations in foraminifera are investigated relative to their ecological preferences and geochemical environment. This study demonstrates that Mn in foraminiferal tests is a promising tool to reconstruct oxygen conditions in the seabed.
Siobhan Williams, Walter Adey, Jochen Halfar, Andreas Kronz, Patrick Gagnon, David Bélanger, and Merinda Nash
Biogeosciences, 15, 5745–5759, https://doi.org/10.5194/bg-15-5745-2018, https://doi.org/10.5194/bg-15-5745-2018, 2018
Robert Frei, Cora Paulukat, Sylvie Bruggmann, and Robert M. Klaebe
Biogeosciences, 15, 4905–4922, https://doi.org/10.5194/bg-15-4905-2018, https://doi.org/10.5194/bg-15-4905-2018, 2018
Short summary
Short summary
The reconstruction of paleo-redox conditions of seawater has the potential to link to climatic changes on land and therefore to contribute to our understanding of past climate change. The redox-sensitive chromium isotope system is applied to marine calcifiers in order to characterize isotope offsets that result from vital processes during calcification processes and which can be eventually used in fossil equivalents to reconstruct past seawater compositions.
Thomas M. DeCarlo, Michael Holcomb, and Malcolm T. McCulloch
Biogeosciences, 15, 2819–2834, https://doi.org/10.5194/bg-15-2819-2018, https://doi.org/10.5194/bg-15-2819-2018, 2018
Short summary
Short summary
Understanding the mechanisms of coral calcification is limited by the isolation of the calcifying environment. The boron systematics (B / Ca and δ11B) of aragonite have recently been developed as a proxy for the carbonate chemistry of the calcifying fluid, but a variety of approaches have been utilized. We assess the available experimental B / Ca partitioning data and present a computer code for deriving calcifying fluid carbonate chemistry from the boron systematics of coral skeletons.
Manuel Bringué, Robert C. Thunell, Vera Pospelova, James L. Pinckney, Oscar E. Romero, and Eric J. Tappa
Biogeosciences, 15, 2325–2348, https://doi.org/10.5194/bg-15-2325-2018, https://doi.org/10.5194/bg-15-2325-2018, 2018
Short summary
Short summary
We document 2.5 yr of dinoflagellate cyst production in the Cariaco Basin using a sediment trap record. Each species' production pattern is interpreted in the context of the physico-chemical (e.g., temperature, nutrients) and biological (other planktonic groups) environment. Most species respond positively to upwelling, but seem to be negatively impacted by an El Niño event with a 1-year lag. This work helps understanding dinoflagellate ecology and interpreting fossil assemblages in sediments.
Gabriella M. Weiss, Eva Y. Pfannerstill, Stefan Schouten, Jaap S. Sinninghe Damsté, and Marcel T. J. van der Meer
Biogeosciences, 14, 5693–5704, https://doi.org/10.5194/bg-14-5693-2017, https://doi.org/10.5194/bg-14-5693-2017, 2017
Short summary
Short summary
Algal-derived compounds allow us to make assumptions about environmental conditions in the past. In order to better understand how organisms record environmental conditions, we grew microscopic marine algae at different light intensities, salinities, and alkalinities in a temperature-controlled environment. We determined how these environmental parameters affected specific algal-derived compounds, especially their relative deuterium content, which seems to be mainly affected by salinity.
S. Nemiah Ladd, Nathalie Dubois, and Carsten J. Schubert
Biogeosciences, 14, 3979–3994, https://doi.org/10.5194/bg-14-3979-2017, https://doi.org/10.5194/bg-14-3979-2017, 2017
Short summary
Short summary
Hydrogen isotopes of lipids provide valuable information about microbial activity, climate, and environmental stress. We show that heavy hydrogen in fatty acids declines from spring to summer in a nutrient-rich and a nutrient-poor lake and that the effect is nearly 3 times as big in the former. This effect is likely a combination of increased biomass from algae, warmer temperatures, and higher algal growth rates.
Karoliina A. Koho, Lennart J. de Nooijer, Christophe Fontanier, Takashi Toyofuku, Kazumasa Oguri, Hiroshi Kitazato, and Gert-Jan Reichart
Biogeosciences, 14, 3067–3082, https://doi.org/10.5194/bg-14-3067-2017, https://doi.org/10.5194/bg-14-3067-2017, 2017
Short summary
Short summary
Here we report Mn / Ca ratios in living benthic foraminifera from the NE Japan margin. The results show that the Mn incorporation directly reflects the environment where the foraminifera calcify. Foraminifera that live deeper in sediment, under greater redox stress, generally incorporate more Mn into their carbonate skeletons. As such, foraminifera living close to the Mn reduction zone in sediment appear promising tools for paleoceanographic reconstructions of sedimentary redox conditions.
Stefania Milano, Gernot Nehrke, Alan D. Wanamaker Jr., Irene Ballesta-Artero, Thomas Brey, and Bernd R. Schöne
Biogeosciences, 14, 1577–1591, https://doi.org/10.5194/bg-14-1577-2017, https://doi.org/10.5194/bg-14-1577-2017, 2017
Diana Zúñiga, Celia Santos, María Froján, Emilia Salgueiro, Marta M. Rufino, Francisco De la Granda, Francisco G. Figueiras, Carmen G. Castro, and Fátima Abrantes
Biogeosciences, 14, 1165–1179, https://doi.org/10.5194/bg-14-1165-2017, https://doi.org/10.5194/bg-14-1165-2017, 2017
Short summary
Short summary
Diatoms are one of the most important primary producers in highly productive coastal regions. Their silicified valves are susceptible to escape from the upper water column and be preserved in the sediment record, and thus are frequently used to reconstruct environmental conditions in the past from sediment cores. Here, we assess how water column diatom’s community in the NW Iberian coastal upwelling system is seasonally transferred from the surface to the seafloor sediments.
Andreia Rebotim, Antje H. L. Voelker, Lukas Jonkers, Joanna J. Waniek, Helge Meggers, Ralf Schiebel, Igaratza Fraile, Michael Schulz, and Michal Kucera
Biogeosciences, 14, 827–859, https://doi.org/10.5194/bg-14-827-2017, https://doi.org/10.5194/bg-14-827-2017, 2017
Short summary
Short summary
Planktonic foraminifera species depth habitat remains poorly constrained and the existing conceptual models are not sufficiently tested by observational data. Here we present a synthesis of living planktonic foraminifera abundance data in the subtropical eastern North Atlantic from vertical plankton tows. We also test potential environmental factors influencing the species depth habitat and investigate yearly or lunar migration cycles. These findings may impact paleoceanographic studies.
Cited articles
Aemisegger, F., Spiegel, J. K., Pfahl, S., Sodemann, H., Eugster, W., and
Wernli, H.: Isotope meteorology of cold front passages: A case study
combining observations and modeling, Geophys. Res. Lett., 42, 5652–5660,
https://doi.org/10.1002/2015GL063988, 2015.
Aleman, J., Leys, B., Apema, R., Bentaleb, I., Dubois, M. A., Lamba, B.,
Lebamba, J., Martin, C., Ngomanda, A., Truc, L., Yangakola, J. M., Favier,
C., and Bremond, L.: Reconstructing savanna tree cover from pollen,
phytoliths and stable carbon isotopes, J. Veg. Sci., 23,
187–197, https://doi.org/10.1111/j.1654-1103.2011.01335.x, 2012.
Alexandre, A., Basile-Doelsch, I., Sonzogni, C., Sylvestre, F., Parron, C.,
Meunier, J. D., and Colin, F.: Oxygen isotope analyses of fine silica grains
using laser-extraction technique: Comparison with oxygen isotope data
obtained from ion microprobe analyses and application to quartzite and
silcrete cement investigation, Geochim. Cosmochim. Ac., 70, 2827–2835,
https://doi.org/10.1016/j.gca.2006.03.003, 2006.
Alexandre, A., Bouvet, M., and Abbadie, L.: The role of savannas in the
terrestrial Si cycle: A case-study from Lamto, Ivory Coast, Glob. Planet.
Change, 78, 162–169, https://doi.org/10.1016/j.gloplacha.2011.06.007, 2011.
Alexandre, A., Crespin, J., Sylvestre, F., Sonzogni, C., and Hilbert, D. W.:
The oxygen isotopic composition of phytolith assemblages from tropical
rainforest soil tops (Queensland, Australia): Validation of a new
paleoenvironmental tool, Clim. Past, 8, 307–324,
https://doi.org/10.5194/cp-8-307-2012, 2012.
Alexandre, A., Landais, A., Vallet-Coulomb, C., Piel, C., Devidal, S.,
Pauchet, S., Sonzogni, C., Couapel, M., Pasturel, M., Cornuault, P., Xin,
J., Mazur, J. C., Prié, F., Bentaleb, I., Webb, E., Chalié, F., and
Roy, J.: The triple oxygen isotope composition of phytoliths as a proxy of
continental atmospheric humidity: Insights from climate chamber and climate
transect calibrations, Biogeosciences, 15, 3223–3241,
https://doi.org/10.5194/bg-15-3223-2018, 2018.
Alexandre, A., Webb, E., Landais, A., Piel, C., Devidal, S., Sonzogni, C.,
Couapel, M., Mazur, J., Pierre, M., Prié, F., Vallet-Coulomb, C.,
Outrequin, C., and Roy, J.: Effects of leaf length and development stage on
the triple oxygen isotope signature of grass leaf water and phytoliths:
insights for a proxy of continental atmospheric humidity, Biogeosciences,
16, 4613–4625, https://doi.org/10.5194/bg-16-4613-2019, 2019.
Aron, P. G., Levin, N. E., Beverly, E. J., Huth, T. E., Passey, B. H.,
Pelletier, E. M., Poulsen, C. J., Winkelstern, I. Z., and Yarian, D. A.:
Triple oxygen isotopes in the water cycle, Chem. Geol., 565, 120026,
https://doi.org/10.1016/j.chemgeo.2020.120026, 2021.
Barbeta, A., Burlett, R., Martín-Gómez, P., Fréjaville, B.,
Devert, N., Wingate, L., Domec, J. C., and Ogée, J.: Evidence for
distinct isotopic compositions of sap and tissue water in tree stems:
consequences for plant water source identification, New Phytol., 233,
1121–1132, https://doi.org/10.1111/nph.17857, 2022.
Barbour, M. M., Loucos, K. E., Lockhart, E. L., Shrestha, A., McCallum, D.,
Simonin, K. A., Song, X., Griffani, D. S., and Farquhar, G. D.: Can
hydraulic design explain patterns of leaf water isotopic enrichment in
C3 plants?, Plant Cell Environ., 44, 432–444,
https://doi.org/10.1111/pce.13943, 2021.
Barkan, E. and Luz, B.: High precision measurements of 17O/16O and
18O
Barkan, E. and Luz, B.: Diffusivity fractionations of
H
Belviso, S., Reiter, I. M., Loubet, B., Gros, V., Lathière, J.,
Montagne, D., Delmotte, M., Ramonet, M., Kalogridis, C., Lebegue, B.,
Bonnaire, N., Kazan, V., Gauquelin, T., Fernandez, C., and Genty, B.: A
top-down approach of surface carbonyl sulfide exchange by a Mediterranean
oak forest ecosystem in southern France, Atmos. Chem. Phys., 16, 14909–14923,
https://doi.org/10.5194/acp-16-14909-2016, 2016.
Benson, L. V. and White, J. W. C.: Stable isotopes of oxygen and hydrogen in
the Truckee River-Pyramid Lake surface-water system, 3. Source of water
vapor overlying Pyramid Lake, Limnol. Oceanogr., 39, 1945–1958,
https://doi.org/10.4319/lo.1994.39.8.1945, 1994.
Blonder, B. and Michaletz, S. T.: A model for leaf temperature decoupling
from air temperature, Agr. Forest. Meteorol., 262, 354–360,
https://doi.org/10.1016/j.agrformet.2018.07.012, 2018.
Bögelein, R., Thomas, F. M., and Kahmen, A.: Leaf water 18O and
2H enrichment along vertical canopy profiles in a broadleaved and a
conifer forest tree, Plant Cell Environ., 40, 1086–1103,
https://doi.org/10.1111/pce.12895, 2017.
Brandriss, M. E., O'Neil, J. R., Edlund, M. B., and Stoermer, E. F.: Oxygen
isotope fractionation between diatomaceous silica and water, Geochim.
Cosmochim. Ac., 62, 1119–1125,
https://doi.org/10.1016/S0016-7037(98)00054-4, 1998.
Bremond, L., Alexandre, A., Peyron, O., and Guiot, J.: Grass water stress
estimated from phytoliths in West Africa, J. Biogeogr., 32, 311–327,
https://doi.org/10.1111/j.1365-2699.2004.01162.x, 2005.
Buhay, W. M., Edwards, T. W. D., and Aravena, R.: Evaluating kinetic
fractionation factors used for reconstructions from oxgen and hydrogen
isotope ratios in plant water and cellulose, Geochim. Cosmochim. Ac., 60,
2209–2218, https://doi.org/10.1016/0016-7037(96)00073-7, 1996.
Bush, R. T., Berke, M. A., and Jacobson, A. D.: Plant Water δD and
δ18O of Tundra Species from West Greenland, Arct. Antarct. Alp
Res., 49, 341–358, https://doi.org/10.1657/AAAR0016-025, 2017.
Cao, X. and Liu, Y.: Equilibrium mass-dependent fractionation relationships
for triple oxygen isotopes, Geochim. Cosmochim. Ac., 75, 7435–7445,
https://doi.org/10.1016/j.gca.2011.09.048, 2011.
Cernusak, L. A., Pate, J. S., and Farquhar, G. D.: Diurnal variation in the
stable isotope composition of water and dry matter in fruiting Lupinus
angustifolius under field conditions, Plant Cell Environ., 25, 893–907,
https://doi.org/10.1046/j.1365-3040.2002.00875.x, 2002.
Cernusak, L. A., Barbour, M. M., Arndt, S. K., Cheesman, A. W., English, N.
B., Feild, T. S., Helliker, B. R., Holloway-Phillips, M. M., Holtum, J. A.
M., Kahmen, A., Mcinerney, F. A., Munksgaard, N. C., Simonin, K. A., Song,
X., Stuart-Williams, H., West, J. B., and Farquhar, G. D.: Stable isotopes
in leaf water of terrestrial plants, Plant Cell Environ., 39, 1087–1102,
https://doi.org/10.1111/pce.12703, 2016.
Chapligin, B., Meyer, H., Friedrichsen, H., Marent, A., Sohns, E., and
Hubberten, H.-W.: A high-performance, safer and semi-automated approach for
the δ18O analysis of diatom silica and new methods for removing
exchangeable oxygen, Rapid Commun. Mass Sp., 24,
2655–2664, https://doi.org/10.1002/rcm.4689, 2010.
Collura, L. V. and Neumann, K.: Wood and bark phytoliths of West African
woody plants, Quaternary Int., 434, 142–159,
https://doi.org/10.1016/j.quaint.2015.12.070, 2017.
Corbineau, R., Reyerson, P. E., Alexandre, A., and Santos, G. M.: Towards
producing pure phytolith concentrates from plants that are suitable for
carbon isotopic analysis, Rev. Palaeobot. Palynol., 197, 179–185,
https://doi.org/10.1016/j.revpalbo.2013.06.001, 2013.
Craig, H. and Gordon, L. I.: Deuterium and oxygen-18 variations in the ocean and the marine atmosphere, in: Stable Isotopes in Oceanographic Studies and Paleotemperatures, edited by: Tongiorgi, E., Spoleto, Consiglio Nazionale Delle Ricerche, Laboratorio di Geologia Nucleare, Pisa, Italy, 9–130, 1965.
Crespin, J., Alexandre, A., Sylvestre, F., Sonzogni, C., Paillès, C.,
and Garreta, V.: IR laser extraction technique applied to oxygen isotope
analysis of small biogenic silica samples, Anal. Chem., 80, 2372–2378,
https://doi.org/10.1021/ac071475c, 2008.
Cuntz, M., Ogée, J., Farquhar, G. D., Peylin, P., and Cernusak, L. A.:
Modelling advection and diffusion of water isotopologues in leaves, Plant
Cell Environ., 30, 892–909,
https://doi.org/10.1111/j.1365-3040.2007.01676.x, 2007.
Diao, H., Schuler, P., Goldsmith, G. R., Siegwolf, R. T., Saurer, M., and
Lehmann, M. M.: Technical note: On uncertainties in plant water isotopic
composition following extraction by cryogenic vacuum distillation, Hydrol.
Earth Syst. Sci., 26, 5835–5847, https://doi.org/10.5194/hess-26-5835-2022,
2022.
Ding, T. P., Zhou, J. X., Wan, D. F., Chen, Z. Y., Wang, C. Y., and Zhang,
F.: Silicon isotope fractionation in bamboo and its significance to the
biogeochemical cycle of silicon, Geochim. Cosmochim. Ac., 72, 1381–1395,
https://doi.org/10.1016/j.gca.2008.01.008, 2008.
Dodd, J. P.: Oxygen isotopes in diatom silica: a new understanding of
silica-water oxygen isotope fractionation in diatom frustules and an
application of diatom δ18O values as a record of
paleohydrologic variability in a Middle-Pleistocene lacustrine core from the
Valles Caldera, New Mexico, 1–108, University of New Mexico, https://digitalrepository.unm.edu/eps_etds/17 (last access: 13 June 2023), 2011.
Dodd, J. P. and Sharp, Z. D.: A laser fluorination method for oxygen isotope
analysis of biogenic silica and a new oxygen isotope calibration of modern
diatoms in freshwater environments, Geochim. Cosmochim. Ac., 74, 1381–1390,
https://doi.org/10.1016/j.gca.2009.11.023, 2010.
Dongmann, G., Nürnberg, H. W., Förstel, H., and Wagener, K.: On the
enrichment of H
Farquhar, G. D. and Cernusak, L. A.: On the isotopic composition of leaf
water in the non-steady state, Funct. Plant Biol., 32, 293–303,
https://doi.org/10.1071/FP04232, 2005.
Farquhar, G. D. and Gan, K. S.: On the progressive enrichment of the oxygen
isotopic, Plant Cell Environ., 26, 1579–1597,
https://doi.org/10.1046/j.1365-3040.2003.01013.x, 2003.
Farquhar, G. D. and Lloyd, J.: Carbon and Oxygen Isotope Effects in the
Exchange of Carbon Dioxide between Terrestrial Plants and the Atmosphere,
in: Stable Isotopes and Plant Carbon-Water Relations, Academic Press,
47–70, https://doi.org/10.1016/B978-0-08-091801-3.50011-8, 1993.
Farquhar, G. D., Cernusak, L. A., and Barnes, B.: Heavy water fractionation
during transpiration, Plant Physiol., 143, 11–18,
https://doi.org/10.1104/pp.106.093278, 2007.
Farris, F. and Strain, B. R.: The effects of water-stress on leaf
H
Fiorella, R. P., West, J. B., and Bowen, G. J.: Biased estimates of the
isotope ratios of steady-state evaporation from the assumption of
equilibrium between vapour and precipitation, Hydrol. Process., 33,
2576–2590, https://doi.org/10.1002/hyp.13531, 2019.
Flanagan, L. B. and Farquhar, G. D.: Variation in the carbon and oxygen
isotope composition of plant biomass and its relationship to water-use
efficiency at the leaf- and ecosystem-scales in a northern Great Plains
grassland, Plant Cell Environ., 37, 425–438,
https://doi.org/10.1111/pce.12165, 2014.
Flanagan, L. B., Comstock, J. P., and Ehleringer, J. R.: Comparison of
Modeled and Observed Environmental Influences on the Stable Oxygen and
Hydrogen Isotope Composition of Leaf Water in Phaseolus vulgaris L., Plant
Physiol., 96, 588–596, https://doi.org/10.1104/pp.96.2.588, 1991.
Gan, K. S., Wong, S. C., Yong, J. W. H., and Farquhar, G. D.: 18O
Spatial Patterns of Vein Xylem Water, Leaf Water, and Dry Matter in Cotton
Leaves, Plant Physiol., 130, 1008–1021, https://doi.org/10.1104/pp.007419,
2002.
Garcin, Y., Schwab, V. F., Gleixner, G., Kahmen, A., Todou, G.,
Séné, O., Onana, J. M., Achoundong, G., and Sachse, D.: Hydrogen
isotope ratios of lacustrine sedimentary n-alkanes as proxies of tropical
African hydrology: Insights from a calibration transect across Cameroon,
Geochim. Cosmochim. Ac., 79, 106–126,
https://doi.org/10.1016/j.gca.2011.11.039, 2012.
Garcin, Y., Schefuß, E., Dargie, G. C., Hawthorne, D., Lawson, I. T.,
Sebag, D., Biddulph, G. E., Crezee, B., Bocko, Y. E., Ifo, S. A., Mampouya
Wenina, Y. E., Mbemba, M., Ewango, C. E. N., Emba, O., Bola, P., Kanyama
Tabu, J., Tyrrell, G., Young, D. M., Gassier, G., Girkin, N. T., Vane, C.
H., Adatte, T., Baird, A. J., Boom, A., Gulliver, P., Morris, P. J., Page,
S. E., Sjögersten, S., and Lewis, S. L.: Hydroclimatic vulnerability of
peat carbon in the central Congo Basin, Nature, 612, 277–282,
https://doi.org/10.1038/s41586-022-05389-3, 2022.
Graf, P., Wernli, H., Pfahl, S., and Sodemann, H.: A new interpretative
framework for below-cloud effects on stable water isotopes in vapour and
rain, Atmos. Chem. Phys., 19, 747–765,
https://doi.org/10.5194/acp-19-747-2019, 2019.
Gröning, M., Lutz, H. O., Roller-Lutz, Z., Kralik, M., Gourcy, L., and
Pöltenstein, L.: A simple rain collector preventing water re-evaporation
dedicated for δ18O and δ2H analysis of cumulative
precipitation samples, J. Hydrol., 448–449, 195–200,
https://doi.org/10.1016/j.jhydrol.2012.04.041, 2012.
Grossiord, C., Buckley, T. N., Cernusak, L. A., Novick, K. A., Poulter, B.,
Siegwolf, R. T. W., Sperry, J. S., and McDowell, N. G.: Plant responses to
rising vapor pressure deficit, New Phytol., 226, 1550–1566,
https://doi.org/10.1111/nph.16485, 2020.
Helliker, B. R. and Ehleringer, J. R.: Establishing a grassland signature in
veins: 18O in the leaf water of C3 and C4 grasses, P. Natl. Acad. Sci. USA, 94,
7894–7898, https://doi.org/10.1073/pnas.97.14.7894, 2000.
Helliker, B. R. and Ehleringer, J. R.: Differential 18O enrichment of
leaf cellulose in C3 versus C4 grasses, Funct. Plant Biol.,
29, 435–442, https://doi.org/10.1071/PP01122, 2002a.
Helliker, B. R. and Ehleringer, J. R.: Grass blades as tree rings:
Environmentally induced changes in the oxygen isotope ratio of cellulose
along the length of grass blades, New Phytol., 155, 417–424,
https://doi.org/10.1046/j.1469-8137.2002.00480.x, 2002b.
Hirl, R. T., Schnyder, H., Ostler, U., Schäufele, R., Schleip, I.,
Vetter, S. H., Auerswald, K., Baca Cabrera, J. C., Wingate, L., Barbour, M.
M., and Ogée, J.: The 18O ecohydrology of a grassland ecosystem –
predictions and observations, Hydrol. Earth Syst. Sci., 23, 2581–2600,
https://doi.org/10.5194/hess-23-2581-2019, 2019.
Holloway-Phillips, M., Cernusak, L. A., Barbour, M., Song, X., Cheesman, A.,
Munksgaard, N., Stuart-Williams, H., and Farquhar, G. D.: Leaf vein fraction
influences the Péclet effect and 18O enrichment in leaf water,
Plant Cell Environ., 39, 2414–2427, https://doi.org/10.1111/pce.12792, 2016.
Hu, G. and Clayton, R. N.: Oxygen isotope salt effects at high pressure and
high temperature and the calibration of oxygen isotope geothermometers,
Geochim. Cosmochim. Ac., 67, 3227–3246,
https://doi.org/10.1016/S0016-7037(02)01319-4, 2003.
IPCC: Climate Change 2013: The Physical Science Basis, Contribution of
Working Group I to the Fifth Assessment Report of the Intergovernmental
Panel on Climate Change, edited by: Stocker, T. F., Qin, D., Plattner,
G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A., Xia, Y., Bex, V.,
and Midgley, P. M., Cambridge University Press, Cambridge, United Kingdom
and New York, NY, USA, 1585 pp., https://doi.org/10.1017/CBO9781107415324, 2013.
IUSS Working Group WRB: World Reference Base for Soil Resources 2014, update
2015. International soil classification system for naming soils and creating
legends for soil maps, World Soil Resources Reports No. 106, FAO, Rome, ISBN 978-92-5-108369-7,
2015.
Jacob, H. and Sonntag, C.: An 8-year record of the seasonal variation of
2H and 18O in atmospheric water vapour and precipitation at
Heidelberg, Germany, Tellus B, 43 291–300,
https://doi.org/10.1034/j.1600-0889.1991.t01-2-00003.x, 1991.
Kahmen, A., Sachse, D., Arndt, S. K., Tu, K. P., Farrington, H., Vitousek,
P. M., and Dawsona, T. E.: Cellulose δ18O is an index of
leaf-to-air vapor pressure difference (VPD) in tropical plants, P. Natl. Acad. Sci. USA, 108,
1981–1986, https://doi.org/10.1073/pnas.1018906108, 2011.
Kahmen, A., Schefuß, E., and Sachse, D.: Leaf water deuterium enrichment
shapes leaf wax n-alkane δD values of angiosperm plants I:
Experimental evidence and mechanistic insights, Geochim. Cosmochim. Ac., 111,
39–49, https://doi.org/10.1016/j.gca.2012.09.003, 2013.
Knauth, L. P. and Epstein, S.: Hydrogen and oxygen isotope ratios in nodular
and bedded cherts, Geochim. Cosmochim. Ac., 40, 95–1108,
https://doi.org/10.1016/0016-7037(76)90051-X, 1976.
Krabbenhoft, D. P., Bowser, C. J., Anderson, M. P., and Valley, J. W.:
Estimating groundwater exchange with lakes: 1. The stable isotope mass
balance method, Water Resour. Res., 26, 2445–2453,
https://doi.org/10.1029/WR026i010p02445, 1990.
Kumar, S., Soukup, M., and Elbaum, R.: Silicification in grasses: Variation
between different cell types, Front. Plant Sci., 8, 1–8,
https://doi.org/10.3389/fpls.2017.00438, 2017.
Landais, A., Risi, C., Bony, S., Vimeux, F., Descroix, L., Falourd, S., and
Bouygues, A.: Combined measurements of 17Oexcess and d-excess in
African monsoon precipitation: Implications for evaluating convective
parameterizations, Earth Planet Sc. Lett., 298, 104–112,
https://doi.org/10.1016/j.epsl.2010.07.033, 2010.
Leaney, F. W., Osmond, C. B., Allison, G. B., and Ziegler, H.:
Hydrogen-isotope composition of leaf water in C3 and C4 plants:
its relationship to the hydrogen-isotope composition of dry matter, Planta,
164, 215–220, https://doi.org/10.1007/BF00396084, 1985.
Lee, X., Smith, R., and Williams, J.: Water vapour 18O
Leuzinger, S. and Körner, C.: Tree species diversity affects canopy leaf
temperatures in a mature temperate forest, Agr. Forest. Meteorol., 146, 29–37,
https://doi.org/10.1016/j.agrformet.2007.05.007, 2007.
Li, S., Levin, N. E., Soderberg, K., Dennis, K. J., and Caylor, K. K.:
Triple oxygen isotope composition of leaf waters in Mpala, central Kenya,
Earth Planet Sc. Lett., 468, 38–50,
https://doi.org/10.1016/j.epsl.2017.02.015, 2017.
Liu, H. T., Schäufele, R., Gong, X. Y., and Schnyder, H.: The δ18O and δ2H of water in the leaf
growth-and-differentiation zone of grasses is close to source water in both
humid and dry atmospheres, New Phytol., 214, 1423–1431,
https://doi.org/10.1111/nph.14549, 2017.
Liu, P., Liu, J., Ji, A., Reinhard, C. T., Planavsky, N. J., Babikov, D.,
Najjar, R. G., and Kasting, J. F.: Triple oxygen isotope constraints on
atmospheric O2 and biological productivity during the mid-Proterozoic,
P. Natl. Acad. Sci USA, 118, e2105074118, https://doi.org/10.1073/pnas.2105074118, 2021.
López, J., Way, D. A., and Sadok, W.: Systemic effects of rising
atmospheric vapor pressure deficit on plant physiology and productivity,
Glob. Change Biol., 27, 1704–1720, https://doi.org/10.1111/gcb.15548, 2021.
Loucos, K. E., Simonin, K. A., Song, X., and Barbour, M. M.: Observed
relationships between leaf H
Luz, B. and Barkan, E.: Variations of 17O
Majoube, M.: Fractionnement en oxygène 18 et en deutérium entre l'eau et sa vapeur, J. Chim. Phys., 68, 1423–1436, https://doi.org/10.1051/jcp/1971681423, 1971.
Merlivat, L.: Molecular diffusivities of H
Monteith, J.: Evaporation and environment, Symp. Soc. Exp. Biol., 19, 205–234,
1965.
Motomura, H., Fujii, T., and Suzuki, M.: Silica deposition in relation to
ageing of leaf tissues in Sasa veitchii (Carrière) Rehder (Poaceae:
Bambusoideae), Ann. Bot., 93, 235–248, https://doi.org/10.1093/aob/mch034,
2004.
Nogué, S., Whicher, K., Baker, A. G., Bhagwat, S. A., and Willis, K. J.:
Phytolith analysis reveals the intensity of past land use change in the
Western Ghats biodiversity hotspot, Quaternary Int., 437, 82–89,
https://doi.org/10.1016/j.quaint.2015.11.113, 2017.
Ogée, J., Cuntz, M., Peylin, P., and Bariac, T.: Non-steady-state,
non-uniform transpiration rate and leaf anatomy effects on the progressive
stable isotope enrichment of leaf water along monocot leaves, Plant Cell
Environ., 30, 367–387, https://doi.org/10.1111/j.1365-3040.2006.01621.x,
2007.
O'Neil, J. R. and Clayton, R. N.: Oxygen isotope geothermometry, in: Isotope and Cosmic Chemistry, edited by: Craig, H. et al., North-Holland, Amsterdam, 157–168, 1964.
Outrequin, C., Alexandre, A., Vallet-Coulomb, C., Piel, C., Devidal, S., Landais, A., Couapel, M., Mazur, J.-C., Peugeot, C., Pierre, M., Prié, F., Roy, J., Sonzogni, C., and Voigt, C.: The triple oxygen isotope composition of phytoliths, a new proxy of atmospheric relative humidity: controls of soil water isotope composition, temperature, CO2 concentration and relative humidity, Clim. Past, 17, 1881–1902, https://doi.org/10.5194/cp-17-1881-2021, 2021.
Penchenat, T., Vimeux, F., Daux, V., Cattani, O., Viale, M., Villalba, R.,
Srur, A., and Outrequin, C.: Isotopic Equilibrium Between Precipitation and
Water Vapor in Northern Patagonia and Its Consequences on δ18O cellulose Estimate, J. Geophys. Res.-Biogeo., 125, e2019JG005418,
https://doi.org/10.1029/2019JG005418, 2020.
Perry, C. C., Williams, R. J. P., and Fry, S. C.: Cell Wall Biosynthesis
during Silicification of Grass Hairs, J. Plant Physiol., 126, 437–448,
https://doi.org/10.1016/S0176-1617(87)80028-7, 1987.
Reiter I. M., Castagnoli G., and Rotereau A.: COOPERATE database, https://cooperate.eccorev.fr/db (last access: 8 June 2022), 2015.
Resco de Dios, V., Chowdhury, F. I., Granda, E., Yao, Y., and Tissue, D. T.:
Assessing the potential functions of nocturnal stomatal conductance in
C3 and C4 plants, New Phytol., 223, 1696–1706,
https://doi.org/10.1111/nph.15881, 2019.
Rey-Sánchez, A. C., Slot, M., Posada, J. M., and Kitajima, K.: Spatial
and seasonal variation in leaf temperature within the canopy of a tropical
forest, Clim. Res., 71, 75–89, https://doi.org/10.3354/cr01427, 2016.
Ripullone, F., Matsuo, N., Stuart-Williams, H., Suan, C. W., Borghetti, M.,
Tani, M., and Farquhar, G.: Environmental effects on oxygen isotope
enrichment of leaf water in cotton leaves, Plant Physiol., 146, 729–736,
https://doi.org/10.1104/pp.107.105643, 2008.
Roden, J. S., Lin, G., and Ehleringer, J. R.: A mechanistic model for
interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose,
Geochim. Cosmochim. Ac., 64, 21–35,
https://doi.org/10.1016/S0016-7037(99)00195-7, 2000.
Sharp, Z. D., Gibbons, J. A., Maltsev, O., Atudorei, V., Pack, A., Sengupta,
S., Shock, E. L., and Knauth, L. P.: A calibration of the triple oxygen
isotope fractionation in the SiO2-H2O system and applications to
natural samples, Geochim. Cosmochim. Ac., 186, 105–119,
https://doi.org/10.1016/j.gca.2016.04.047, 2016.
Shemesh, A., Charles, C. D., and Fairbanks, R. G.: Oxygen Isotopes in
Biogenic Silica: Global Changes in Ocean Temperature and Isotopic
Composition, Science, 256, 1434–1436,
https://doi.org/10.1126/science.256.5062.1434, 1992.
Siebert, S., Ewert, F., Eyshi Rezaei, E., Kage, H., and Graß, R.: Impact
of heat stress on crop yield – On the importance of considering canopy
temperature, Environ. Res. Lett., 9, 044012,
https://doi.org/10.1088/1748-9326/9/4/044012, 2014.
Song, X., Barbour, M. M., Saurer, M., and Helliker, B. R.: Examining the
large-scale convergence of photosynthesis-weighted tree leaf temperatures
through stable oxygen isotope analysis of multiple data sets, New
Phytol., 192, 912–924,
https://doi.org/10.1111/j.1469-8137.2011.03851.x, 2011.
Song, X., Simonin, K. A., Loucos, K. E., and Barbour, M. M.: Modelling
non-steady-state isotope enrichment of leaf water in a gas-exchange cuvette
environment, Plant Cell Environ., 38, 2618–2628,
https://doi.org/10.1111/pce.12571, 2015.
Still, C., Powell, R., Aubrecht, D., Kim, Y., Helliker, B., Roberts, D.,
Richardson, A. D., and Goulden, M.: Thermal imaging in plant and ecosystem
ecology: applications and challenges, Ecosphere, 10, e02768,
https://doi.org/10.1002/ecs2.2768, 2019.
Surma, J., Assonov, S., Bolourchi, M. J., and Staubwasser, M.: Triple oxygen
isotope signatures in evaporated water bodies from the Sistan Oasis, Iran,
Geophys. Res. Lett., 42, 8456–8462, https://doi.org/10.1002/2015GL066475,
2015.
Surma, J., Assonov, S., and Staubwasser, M.: Triple Oxygen Isotope
Systematics in the Hydrologic Cycle, Rev. Mineral. Geochem., 86, 401–428,
https://doi.org/10.2138/rmg.2021.86.12, 2021.
Tierney, J. E., Poulsen, C. J., Montañez, I. P., Bhattacharya, T., Feng,
R., Ford, H. L., Hönisch, B., Inglis, G. N., Petersen, S. V., Sagoo, N.,
Tabor, C. R., Thirumalai, K., Zhu, J., Burls, N. J., Foster, G. L.,
Goddéris, Y., Huber, B. T., Ivany, L. C., Turner, S. K., Lunt, D. J.,
McElwain, J. C., Mills, B. J. W., Otto-Bliesner, B. L., Ridgwell, A., and
Zhang, Y. G.: Past climates inform our future, Science, 370, eaay3701,
https://doi.org/10.1126/science.aay3701, 2020.
Tobin, R. L. and Kulmatiski, A.: Plant identity and shallow soil moisture
are primary drivers of stomatal conductance in the savannas of Kruger
National Park, PLoS One, 13, 1–17,
https://doi.org/10.1371/journal.pone.0191396, 2018.
Treydte, K., Boda, S., Graf Pannatier, E., Fonti, P., Frank, D., Ullrich,
B., Saurer, M., Siegwolf, R., Battipaglia, G., Werner, W., and Gessler, A.:
Seasonal transfer of oxygen isotopes from precipitation and soil to the tree
ring: Source water versus needle water enrichment, New Phytol., 202,
772–783, https://doi.org/10.1111/nph.12741, 2014.
Tsujimura, M., Sasaki, L., Yamanaka, T., Sugimoto, A., Li, S. G.,
Matsushima, D., Kotani, A., and Saandar, M.: Vertical distribution of stable
isotopic composition in atmospheric water vapor and subsurface water in
grassland and forest sites, eastern Mongolia, J. Hydrol., 333, 35–46,
https://doi.org/10.1016/j.jhydrol.2006.07.025, 2007.
Tuthorn, M., Zech, R., Ruppenthal, M., Oelmann, Y., Kahmen, A., del Valle,
H. F., Eglinton, T., Rozanski, K., and Zech, M.: Coupling δ2H
and δ18O biomarker results yields information on relative
humidity and isotopic composition of precipitation – a climate transect
validation study, Biogeosciences, 12, 3913–3924,
https://doi.org/10.5194/bg-12-3913-2015, 2015.
Vallet-Coulomb, C., Couapel, M., and Sonzogni, C.: Improving memory effect
correction to achieve high precision analysis of δ17O, δ18O δ2H, 17O-excess and d-excess in water using
cavity ring-down laser spectroscopy, Rapid Commun. Mass
Sp., 35, e9108, https://doi.org/10.1002/rcm.9108, 2021.
Voelker, S. L., Brooks, J. R., Meinzer, F. C., Roden, J., Pazdur, A.,
Pawelczyk, S., Hartsough, P., Snyder, K., Plavcová, L., and
Šantruček, J.: Reconstructing relative humidity from plant δ18O and δD as deuterium deviations from the global meteoric
water line, Ecol. Appl., 24, 960–975,
https://doi.org/10.1890/13-0988.1, 2014.
Voigt, C., Herwartz, D., Dorador, C., and Staubwasser, M.: Triple oxygen
isotope systematics of evaporation and mixing processes in a dynamic desert
lake system, Hydrol. Earth Syst. Sci., 25, 1211–1228,
https://doi.org/10.5194/hess-25-1211-2021, 2021.
Voigt, C., Vallet-Coulomb, C., Piel, C., and Alexandre, A.: 17O-excess
and d-excess of atmospheric water vapor measured by cavity ring-down
spectrometry: Evidence of a matrix effect and implication for the
calibration procedure, Rapid Commun. Mass Sp., 36, e9227,
https://doi.org/10.1002/rcm.9227, 2022.
Wang, P., Yamanaka, T., Li, X. Y., Wu, X., Chen, B., Liu, Y., Wei, Z., and
Ma, W.: A multiple time scale modeling investigation of leaf water isotope
enrichment in a temperate grassland ecosystem, Ecol. Res., 33, 901–915,
https://doi.org/10.1007/s11284-018-1591-3, 2018.
Webb, E. A. and Longstaffe, F. J.: The oxygen isotopic compositions of
silica phytoliths and plant water in grasses: Implications for the study of
paleoclimate, Geochim. Cosmochim. Ac., 64, 767–780,
https://doi.org/10.1016/S0016-7037(99)00374-9, 2000.
Webb, E. A. and Longstaffe, F. J.: Climatic influences on the oxygen
isotopic composition of biogenic silica in prairie grass, Geochim. Cosmochim.
Ac., 66, 1891–1904, https://doi.org/10.1016/S0016-7037(02)00822-0, 2002.
Webb, E. A. and Longstaffe, F. J.: Identifying the δ18O
signature of precipitation in grass cellulose and phytoliths: Refining the
paleoclimate model, Geochim. Cosmochim. Ac., 70, 2417–2426,
https://doi.org/10.1016/j.gca.2006.02.024, 2006.
Wen, X. F., Zhang, S. C., Sun, X., Yu, G., and Lee, X.: Water vapor and
precipitation isotope ratios in Beijing, China, J. Geophys.
Res.-Atmos., 115, 1–10, https://doi.org/10.1029/2009JD012408,
2010.
Yakir, D., Berry, J. A., Giles, L., and Osmond, C. B.: Isotopic
heterogeneity of water in transpiring leaves: identification of the
component that controls the δ18O of atmospheric O2 and
CO2, Plant Cell Environ., 17, 73–80,
https://doi.org/10.1111/j.1365-3040.1994.tb00267.x, 1994.
Zech, M., Mayr, C., Tuthorn, M., Leiber-Sauheitl, K., and Glaser, B.: Oxygen
isotope ratios (18O
Short summary
Data on past relative humidity (RH) ARE needed to improve its representation in Earth system models. A novel isotope parameter (17O-excess) of plant silica has been developed to quantify past RH. Using comprehensive monitoring and novel methods, we show how environmental and plant physiological parameters influence the 17O-excess of plant silica and leaf water, i.e. its source water. The insights gained from this study will help to improve estimates of RH from fossil plant silica deposits.
Data on past relative humidity (RH) ARE needed to improve its representation in Earth system...
Altmetrics
Final-revised paper
Preprint