Articles | Volume 21, issue 7
https://doi.org/10.5194/bg-21-1629-2024
© Author(s) 2024. 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-21-1629-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
BG Letters
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04 Apr 2024
BG Letters | Highlight paper |
| 04 Apr 2024
| 04 Apr 2024
Rates of palaeoecological change can inform ecosystem restoration
Walter Finsinger
CORRESPONDING AUTHOR
ISEM, University of Montpellier, CNRS, IRD, Montpellier, 34095, France
Christian Bigler
Department of Ecology and Environmental Science, Umeå University, Umeå, 90187, Sweden
Christoph Schwörer
Institute of Plant Sciences and Oeschger Centre for Climate Change Research, University of Bern, 3013 Bern, Switzerland
Willy Tinner
Institute of Plant Sciences and Oeschger Centre for Climate Change Research, University of Bern, 3013 Bern, Switzerland
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Jack Longman, Daniel Veres, Aritina Haliuc, Walter Finsinger, Vasile Ersek, Daniela Pascal, Tiberiu Sava, and Robert Begy
Clim. Past, 17, 2633–2652, https://doi.org/10.5194/cp-17-2633-2021, https://doi.org/10.5194/cp-17-2633-2021, 2021
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Peatlands are some of the best environments for storing carbon; thus, comprehending how much carbon can be stored and how amounts have changed through time is important to understand carbon cycling. We analysed nine peatlands from central–eastern Europe to look at how carbon storage in mountain bogs has changed over the last 10 000 years. We conclude that human activity is the main driver of changes in storage levels over the past 4000 years; prior to this, climate was the primary driver.
Basil A. S. Davis, Manuel Chevalier, Philipp Sommer, Vachel A. Carter, Walter Finsinger, Achille Mauri, Leanne N. Phelps, Marco Zanon, Roman Abegglen, Christine M. Åkesson, Francisca Alba-Sánchez, R. Scott Anderson, Tatiana G. Antipina, Juliana R. Atanassova, Ruth Beer, Nina I. Belyanina, Tatiana A. Blyakharchuk, Olga K. Borisova, Elissaveta Bozilova, Galina Bukreeva, M. Jane Bunting, Eleonora Clò, Daniele Colombaroli, Nathalie Combourieu-Nebout, Stéphanie Desprat, Federico Di Rita, Morteza Djamali, Kevin J. Edwards, Patricia L. Fall, Angelica Feurdean, William Fletcher, Assunta Florenzano, Giulia Furlanetto, Emna Gaceur, Arsenii T. Galimov, Mariusz Gałka, Iria García-Moreiras, Thomas Giesecke, Roxana Grindean, Maria A. Guido, Irina G. Gvozdeva, Ulrike Herzschuh, Kari L. Hjelle, Sergey Ivanov, Susanne Jahns, Vlasta Jankovska, Gonzalo Jiménez-Moreno, Monika Karpińska-Kołaczek, Ikuko Kitaba, Piotr Kołaczek, Elena G. Lapteva, Małgorzata Latałowa, Vincent Lebreton, Suzanne Leroy, Michelle Leydet, Darya A. Lopatina, José Antonio López-Sáez, André F. Lotter, Donatella Magri, Elena Marinova, Isabelle Matthias, Anastasia Mavridou, Anna Maria Mercuri, Jose Manuel Mesa-Fernández, Yuri A. Mikishin, Krystyna Milecka, Carlo Montanari, César Morales-Molino, Almut Mrotzek, Castor Muñoz Sobrino, Olga D. Naidina, Takeshi Nakagawa, Anne Birgitte Nielsen, Elena Y. Novenko, Sampson Panajiotidis, Nata K. Panova, Maria Papadopoulou, Heather S. Pardoe, Anna Pędziszewska, Tatiana I. Petrenko, María J. Ramos-Román, Cesare Ravazzi, Manfred Rösch, Natalia Ryabogina, Silvia Sabariego Ruiz, J. Sakari Salonen, Tatyana V. Sapelko, James E. Schofield, Heikki Seppä, Lyudmila Shumilovskikh, Normunds Stivrins, Philipp Stojakowits, Helena Svobodova Svitavska, Joanna Święta-Musznicka, Ioan Tantau, Willy Tinner, Kazimierz Tobolski, Spassimir Tonkov, Margarita Tsakiridou, Verushka Valsecchi, Oksana G. Zanina, and Marcelina Zimny
Earth Syst. Sci. Data, 12, 2423–2445, https://doi.org/10.5194/essd-12-2423-2020, https://doi.org/10.5194/essd-12-2423-2020, 2020
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The Eurasian Modern Pollen Database (EMPD) contains pollen counts and associated metadata for 8134 modern pollen samples from across the Eurasian region. The EMPD is part of, and complementary to, the European Pollen Database (EPD) which contains data on fossil pollen found in Late Quaternary sedimentary archives. The purpose of the EMPD is to provide calibration datasets and other data to support palaeoecological research on past climates and vegetation cover over the Quaternary period.
Angelica Feurdean, Boris Vannière, Walter Finsinger, Dan Warren, Simon C. Connor, Matthew Forrest, Johan Liakka, Andrei Panait, Christian Werner, Maja Andrič, Premysl Bobek, Vachel A. Carter, Basil Davis, Andrei-Cosmin Diaconu, Elisabeth Dietze, Ingo Feeser, Gabriela Florescu, Mariusz Gałka, Thomas Giesecke, Susanne Jahns, Eva Jamrichová, Katarzyna Kajukało, Jed Kaplan, Monika Karpińska-Kołaczek, Piotr Kołaczek, Petr Kuneš, Dimitry Kupriyanov, Mariusz Lamentowicz, Carsten Lemmen, Enikö K. Magyari, Katarzyna Marcisz, Elena Marinova, Aidin Niamir, Elena Novenko, Milena Obremska, Anna Pędziszewska, Mirjam Pfeiffer, Anneli Poska, Manfred Rösch, Michal Słowiński, Miglė Stančikaitė, Marta Szal, Joanna Święta-Musznicka, Ioan Tanţău, Martin Theuerkauf, Spassimir Tonkov, Orsolya Valkó, Jüri Vassiljev, Siim Veski, Ildiko Vincze, Agnieszka Wacnik, Julian Wiethold, and Thomas Hickler
Biogeosciences, 17, 1213–1230, https://doi.org/10.5194/bg-17-1213-2020, https://doi.org/10.5194/bg-17-1213-2020, 2020
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Our study covers the full Holocene (the past 11 500 years) climate variability and vegetation composition and provides a test on how vegetation and climate interact to determine fire hazard. An important implication of this test is that percentage of tree cover can be used as a predictor of the probability of fire occurrence. Biomass burned is highest at ~ 45 % tree cover in temperate forests and at ~ 60–65 % tree cover in needleleaf-dominated forests.
Jack Longman, Daniel Veres, Aritina Haliuc, Walter Finsinger, Vasile Ersek, Daniela Pascal, Tiberiu Sava, and Robert Begy
Clim. Past, 17, 2633–2652, https://doi.org/10.5194/cp-17-2633-2021, https://doi.org/10.5194/cp-17-2633-2021, 2021
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Peatlands are some of the best environments for storing carbon; thus, comprehending how much carbon can be stored and how amounts have changed through time is important to understand carbon cycling. We analysed nine peatlands from central–eastern Europe to look at how carbon storage in mountain bogs has changed over the last 10 000 years. We conclude that human activity is the main driver of changes in storage levels over the past 4000 years; prior to this, climate was the primary driver.
Dimitri Osmont, Sandra Brugger, Anina Gilgen, Helga Weber, Michael Sigl, Robin L. Modini, Christoph Schwörer, Willy Tinner, Stefan Wunderle, and Margit Schwikowski
The Cryosphere, 14, 3731–3745, https://doi.org/10.5194/tc-14-3731-2020, https://doi.org/10.5194/tc-14-3731-2020, 2020
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In this interdisciplinary case study, we were able to link biomass burning emissions from the June 2017 wildfires in Portugal to their deposition in the snowpack at Jungfraujoch, Swiss Alps. We analysed black carbon and charcoal in the snowpack, calculated backward trajectories, and monitored the fire evolution by remote sensing. Such case studies help to understand the representativity of biomass burning records in ice cores and how biomass burning tracers are archived in the snowpack.
Basil A. S. Davis, Manuel Chevalier, Philipp Sommer, Vachel A. Carter, Walter Finsinger, Achille Mauri, Leanne N. Phelps, Marco Zanon, Roman Abegglen, Christine M. Åkesson, Francisca Alba-Sánchez, R. Scott Anderson, Tatiana G. Antipina, Juliana R. Atanassova, Ruth Beer, Nina I. Belyanina, Tatiana A. Blyakharchuk, Olga K. Borisova, Elissaveta Bozilova, Galina Bukreeva, M. Jane Bunting, Eleonora Clò, Daniele Colombaroli, Nathalie Combourieu-Nebout, Stéphanie Desprat, Federico Di Rita, Morteza Djamali, Kevin J. Edwards, Patricia L. Fall, Angelica Feurdean, William Fletcher, Assunta Florenzano, Giulia Furlanetto, Emna Gaceur, Arsenii T. Galimov, Mariusz Gałka, Iria García-Moreiras, Thomas Giesecke, Roxana Grindean, Maria A. Guido, Irina G. Gvozdeva, Ulrike Herzschuh, Kari L. Hjelle, Sergey Ivanov, Susanne Jahns, Vlasta Jankovska, Gonzalo Jiménez-Moreno, Monika Karpińska-Kołaczek, Ikuko Kitaba, Piotr Kołaczek, Elena G. Lapteva, Małgorzata Latałowa, Vincent Lebreton, Suzanne Leroy, Michelle Leydet, Darya A. Lopatina, José Antonio López-Sáez, André F. Lotter, Donatella Magri, Elena Marinova, Isabelle Matthias, Anastasia Mavridou, Anna Maria Mercuri, Jose Manuel Mesa-Fernández, Yuri A. Mikishin, Krystyna Milecka, Carlo Montanari, César Morales-Molino, Almut Mrotzek, Castor Muñoz Sobrino, Olga D. Naidina, Takeshi Nakagawa, Anne Birgitte Nielsen, Elena Y. Novenko, Sampson Panajiotidis, Nata K. Panova, Maria Papadopoulou, Heather S. Pardoe, Anna Pędziszewska, Tatiana I. Petrenko, María J. Ramos-Román, Cesare Ravazzi, Manfred Rösch, Natalia Ryabogina, Silvia Sabariego Ruiz, J. Sakari Salonen, Tatyana V. Sapelko, James E. Schofield, Heikki Seppä, Lyudmila Shumilovskikh, Normunds Stivrins, Philipp Stojakowits, Helena Svobodova Svitavska, Joanna Święta-Musznicka, Ioan Tantau, Willy Tinner, Kazimierz Tobolski, Spassimir Tonkov, Margarita Tsakiridou, Verushka Valsecchi, Oksana G. Zanina, and Marcelina Zimny
Earth Syst. Sci. Data, 12, 2423–2445, https://doi.org/10.5194/essd-12-2423-2020, https://doi.org/10.5194/essd-12-2423-2020, 2020
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The Eurasian Modern Pollen Database (EMPD) contains pollen counts and associated metadata for 8134 modern pollen samples from across the Eurasian region. The EMPD is part of, and complementary to, the European Pollen Database (EPD) which contains data on fossil pollen found in Late Quaternary sedimentary archives. The purpose of the EMPD is to provide calibration datasets and other data to support palaeoecological research on past climates and vegetation cover over the Quaternary period.
Fabian Rey, Erika Gobet, Christoph Schwörer, Albert Hafner, Sönke Szidat, and Willy Tinner
Clim. Past, 16, 1347–1367, https://doi.org/10.5194/cp-16-1347-2020, https://doi.org/10.5194/cp-16-1347-2020, 2020
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We present a novel post Last Glacial Maximum sediment record from Moossee (Swiss Plateau, southern central Europe). For the first time, five major reorganizations of vegetation could be definitely linked to paramount postglacial temperature and/or moisture changes. Present-day beech-dominated forests have been resilient to long-term climate change and human land use. They may prevail in future if climate warming does not exceed the amplitude of Mid Holocene temperature and moisture variability.
Angelica Feurdean, Boris Vannière, Walter Finsinger, Dan Warren, Simon C. Connor, Matthew Forrest, Johan Liakka, Andrei Panait, Christian Werner, Maja Andrič, Premysl Bobek, Vachel A. Carter, Basil Davis, Andrei-Cosmin Diaconu, Elisabeth Dietze, Ingo Feeser, Gabriela Florescu, Mariusz Gałka, Thomas Giesecke, Susanne Jahns, Eva Jamrichová, Katarzyna Kajukało, Jed Kaplan, Monika Karpińska-Kołaczek, Piotr Kołaczek, Petr Kuneš, Dimitry Kupriyanov, Mariusz Lamentowicz, Carsten Lemmen, Enikö K. Magyari, Katarzyna Marcisz, Elena Marinova, Aidin Niamir, Elena Novenko, Milena Obremska, Anna Pędziszewska, Mirjam Pfeiffer, Anneli Poska, Manfred Rösch, Michal Słowiński, Miglė Stančikaitė, Marta Szal, Joanna Święta-Musznicka, Ioan Tanţău, Martin Theuerkauf, Spassimir Tonkov, Orsolya Valkó, Jüri Vassiljev, Siim Veski, Ildiko Vincze, Agnieszka Wacnik, Julian Wiethold, and Thomas Hickler
Biogeosciences, 17, 1213–1230, https://doi.org/10.5194/bg-17-1213-2020, https://doi.org/10.5194/bg-17-1213-2020, 2020
Short summary
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Our study covers the full Holocene (the past 11 500 years) climate variability and vegetation composition and provides a test on how vegetation and climate interact to determine fire hazard. An important implication of this test is that percentage of tree cover can be used as a predictor of the probability of fire occurrence. Biomass burned is highest at ~ 45 % tree cover in temperate forests and at ~ 60–65 % tree cover in needleleaf-dominated forests.
Anina Gilgen, Carole Adolf, Sandra O. Brugger, Luisa Ickes, Margit Schwikowski, Jacqueline F. N. van Leeuwen, Willy Tinner, and Ulrike Lohmann
Atmos. Chem. Phys., 18, 11813–11829, https://doi.org/10.5194/acp-18-11813-2018, https://doi.org/10.5194/acp-18-11813-2018, 2018
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Microscopic charcoal particles are fire-specific tracers, which are presently the primary source for reconstructing past fire activity. In this study, we implement microscopic charcoal particles into a global aerosol–climate model to better understand the transport of charcoal on a large scale. We find that the model captures a significant portion of the spatial variability but fails to reproduce the extreme variability observed in the charcoal data.
Related subject area
Biodiversity and Ecosystem Function: Paleo
Comment on “The Volyn biota (Ukraine) – indications of 1.5 Gyr old eukaryotes in 3D preservation, a spotlight on the `boring billion' ” by Franz et al. (2023)
Reply to Comment on Franz et al. (2023): A reinterpretation of the 1.5 billion year old Volyn ‘biota’ of Ukraine, and discussion of the evolution of the eukaryotes, by Head et al. (2023)
Ecological evolution in northern Iberia (SW Europe) during the Late Pleistocene through isotopic analysis on ungulate teeth
Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion
Late Neogene evolution of modern deep-dwelling plankton
Photosynthetic activity in Devonian Foraminifera
Microbial activity, methane production, and carbon storage in Early Holocene North Sea peats
Planktonic foraminifera-derived environmental DNA extracted from abyssal sediments preserves patterns of plankton macroecology
Ecosystem regimes and responses in a coupled ancient lake system from MIS 5b to present: the diatom record of lakes Ohrid and Prespa
Metagenomic analyses of the late Pleistocene permafrost – additional tools for reconstruction of environmental conditions
Differential resilience of ancient sister lakes Ohrid and Prespa to environmental disturbances during the Late Pleistocene
Stable isotope study of a new chondrichthyan fauna (Kimmeridgian, Porrentruy, Swiss Jura): an unusual freshwater-influenced isotopic composition for the hybodont shark Asteracanthus
Amelioration of marine environments at the Smithian–Spathian boundary, Early Triassic
Weathering by tree-root-associating fungi diminishes under simulated Cenozoic atmospheric CO2 decline
The impact of land-use change on floristic diversity at regional scale in southern Sweden 600 BC–AD 2008
Climate-related changes in peatland carbon accumulation during the last millennium
Stratigraphy and paleoenvironments of the early to middle Holocene Chipalamawamba Beds (Malawi Basin, Africa)
Experimental mineralization of crustacean eggs: new implications for the fossilization of Precambrian–Cambrian embryos
The last glacial-interglacial cycle in Lake Ohrid (Macedonia/Albania): testing diatom response to climate
Martin J. Head, James B. Riding, Jennifer M. K. O'Keefe, Julius Jeiter, and Julia Gravendyck
Biogeosciences, 21, 1773–1783, https://doi.org/10.5194/bg-21-1773-2024, https://doi.org/10.5194/bg-21-1773-2024, 2024
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A diverse suite of “fossils” associated with the ~1.5 Ga Volyn (Ukraine) kerite was published recently. We show that at least some of them represent modern contamination including plant hairs, pollen, and likely later fungal growth. Comparable diversity is shown to exist in moderm museum dust, calling into question whether any part of the Volyn biota is of biological origin while emphasising the need for scrupulous care in collecting, analysing, and identifying Precambrian microfossils.
Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chornousenko, and Ulrich Struck
EGUsphere, https://doi.org/10.5194/egusphere-2024-217, https://doi.org/10.5194/egusphere-2024-217, 2024
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The Volyn biota (Ukraine), previously assumed to be an extreme case of natural, abiotic synthesis of organic matter, is more likely a diverse assemblage of fossils from the deep biosphere. Although contamination by modern organisms cannot completely be ruled out, it is unlikely, considering all aspects, i. e. their mode of occurrence in the deep biosphere, their fossilization and mature state of organic matter, their isotope signature, and their large morphological diversity.
Monica Fernández-Garcia, Sarah Pederzani, Kate Britton, Lucia Agudo-Pérez, Andrea Cicero, Jeanne Geiling, Joan Daura, Montse Sanz-Borrás, and Ana B. Marín-Arroyo
Biogeosciences Discuss., https://doi.org/10.5194/bg-2023-128, https://doi.org/10.5194/bg-2023-128, 2023
Revised manuscript accepted for BG
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Significant climatic changes affected Europe's landscape, animals, and human groups during the Late Pleistocene. Reconstructing the local conditions humans faced is essential to understand adaptation processes and resilience. This study analyzed the chemical composition of animal teeth consumed by humans in northern Iberia, spanning 80,000 to 15,000 years, revealing the ecological changing conditios.
Adam Woodhouse, Frances A. Procter, Sophie L. Jackson, Robert A. Jamieson, Robert J. Newton, Philip F. Sexton, and Tracy Aze
Biogeosciences, 20, 121–139, https://doi.org/10.5194/bg-20-121-2023, https://doi.org/10.5194/bg-20-121-2023, 2023
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This study looked into the regional and global response of planktonic foraminifera to the climate over the last 5 million years, when the Earth cooled significantly. These single celled organisms exhibit the best fossil record available to science. We document an abundance switch from warm water to cold water species as the Earth cooled. Moreover, a closer analysis of certain species may indicate higher fossil diversity than previously thought, which has implications for evolutionary studies.
Flavia Boscolo-Galazzo, Amy Jones, Tom Dunkley Jones, Katherine A. Crichton, Bridget S. Wade, and Paul N. Pearson
Biogeosciences, 19, 743–762, https://doi.org/10.5194/bg-19-743-2022, https://doi.org/10.5194/bg-19-743-2022, 2022
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Deep-living organisms are a major yet poorly known component of ocean biomass. Here we reconstruct the evolution of deep-living zooplankton and phytoplankton. Deep-dwelling zooplankton and phytoplankton did not occur 15 Myr ago, when the ocean was several degrees warmer than today. Deep-dwelling species first evolve around 7.5 Myr ago, following global climate cooling. Their evolution was driven by colder ocean temperatures allowing more food, oxygen, and light at depth.
Zofia Dubicka, Maria Gajewska, Wojciech Kozłowski, Pamela Hallock, and Johann Hohenegger
Biogeosciences, 18, 5719–5728, https://doi.org/10.5194/bg-18-5719-2021, https://doi.org/10.5194/bg-18-5719-2021, 2021
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Benthic foraminifera play a significant role in modern reefal ecosystems mainly due to their symbiosis with photosynthetic microorganisms. Foraminifera were also components of Devonian stromatoporoid coral reefs; however, whether they could have harbored symbionts has remained unclear. We show that Devonian foraminifera may have stayed photosynthetically active, which likely had an impact on their evolutionary radiation and possibly also on the functioning of Paleozoic shallow marine ecosystems.
Tanya J. R. Lippmann, Michiel H. in 't Zandt, Nathalie N. L. Van der Putten, Freek S. Busschers, Marc P. Hijma, Pieter van der Velden, Tim de Groot, Zicarlo van Aalderen, Ove H. Meisel, Caroline P. Slomp, Helge Niemann, Mike S. M. Jetten, Han A. J. Dolman, and Cornelia U. Welte
Biogeosciences, 18, 5491–5511, https://doi.org/10.5194/bg-18-5491-2021, https://doi.org/10.5194/bg-18-5491-2021, 2021
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This paper is a step towards understanding the basal peat ecosystem beneath the North Sea. Plant remains followed parallel sequences. Methane concentrations were low with local exceptions, with the source likely being trapped pockets of millennia-old methane. Microbial community structure indicated the absence of a biofilter and was diverse across sites. Large carbon stores in the presence of methanogens and in the absence of methanotrophs have the potential to be metabolized into methane.
Raphaël Morard, Franck Lejzerowicz, Kate F. Darling, Béatrice Lecroq-Bennet, Mikkel Winther Pedersen, Ludovic Orlando, Jan Pawlowski, Stefan Mulitza, Colomban de Vargas, and Michal Kucera
Biogeosciences, 14, 2741–2754, https://doi.org/10.5194/bg-14-2741-2017, https://doi.org/10.5194/bg-14-2741-2017, 2017
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The exploitation of deep-sea sedimentary archive relies on the recovery of mineralized skeletons of pelagic organisms. Planktonic groups leaving preserved remains represent only a fraction of the total marine diversity. Environmental DNA left by non-fossil organisms is a promising source of information for paleo-reconstructions. Here we show how planktonic-derived environmental DNA preserves ecological structure of planktonic communities. We use planktonic foraminifera as a case study.
Aleksandra Cvetkoska, Elena Jovanovska, Alexander Francke, Slavica Tofilovska, Hendrik Vogel, Zlatko Levkov, Timme H. Donders, Bernd Wagner, and Friederike Wagner-Cremer
Biogeosciences, 13, 3147–3162, https://doi.org/10.5194/bg-13-3147-2016, https://doi.org/10.5194/bg-13-3147-2016, 2016
Elizaveta Rivkina, Lada Petrovskaya, Tatiana Vishnivetskaya, Kirill Krivushin, Lyubov Shmakova, Maria Tutukina, Arthur Meyers, and Fyodor Kondrashov
Biogeosciences, 13, 2207–2219, https://doi.org/10.5194/bg-13-2207-2016, https://doi.org/10.5194/bg-13-2207-2016, 2016
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A comparative analysis of the metagenomes from two 30,000-year-old permafrost samples, one of lake-alluvial origin and the other from late Pleistocene Ice Complex sediments, revealed significant differences within microbial communities. The late Pleistocene Ice Complex sediments (which are characterized by the absence of methane with lower values of redox potential and Fe2+ content) showed both a low abundance of methanogenic archaea and enzymes from the carbon, nitrogen, and sulfur cycles.
Elena Jovanovska, Aleksandra Cvetkoska, Torsten Hauffe, Zlatko Levkov, Bernd Wagner, Roberto Sulpizio, Alexander Francke, Christian Albrecht, and Thomas Wilke
Biogeosciences, 13, 1149–1161, https://doi.org/10.5194/bg-13-1149-2016, https://doi.org/10.5194/bg-13-1149-2016, 2016
L. Leuzinger, L. Kocsis, J.-P. Billon-Bruyat, S. Spezzaferri, and T. Vennemann
Biogeosciences, 12, 6945–6954, https://doi.org/10.5194/bg-12-6945-2015, https://doi.org/10.5194/bg-12-6945-2015, 2015
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We measured the oxygen isotopic composition of Late Jurassic chondrichthyan teeth (sharks, rays, chimaeras) from the Swiss Jura to get ecological information. The main finding is that the extinct shark Asteracanthus (Hybodontiformes) could inhabit reduced salinity areas, although previous studies on other European localities always resulted in a clear marine isotopic signal for this genus. We propose a mainly marine ecology coupled with excursions into areas of lower salinity in our study site.
L. Zhang, L. Zhao, Z.-Q. Chen, T. J. Algeo, Y. Li, and L. Cao
Biogeosciences, 12, 1597–1613, https://doi.org/10.5194/bg-12-1597-2015, https://doi.org/10.5194/bg-12-1597-2015, 2015
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The Smithian--Spathian boundary was a key event in the recovery of marine environments and ecosystems following the end-Permian mass extinction ~1.5 million years earlier. Our analysis of the Shitouzhai section in South China reveals major changes in oceanographic conditions at the SSB intensification of oceanic circulation leading to enhanced upwelling of nutrient- and sulfide-rich deep waters and coinciding with an abrupt cooling that terminated the Early Triassic hothouse climate.
J. Quirk, J. R. Leake, S. A. Banwart, L. L. Taylor, and D. J. Beerling
Biogeosciences, 11, 321–331, https://doi.org/10.5194/bg-11-321-2014, https://doi.org/10.5194/bg-11-321-2014, 2014
D. Fredh, A. Broström, M. Rundgren, P. Lagerås, F. Mazier, and L. Zillén
Biogeosciences, 10, 3159–3173, https://doi.org/10.5194/bg-10-3159-2013, https://doi.org/10.5194/bg-10-3159-2013, 2013
D. J. Charman, D. W. Beilman, M. Blaauw, R. K. Booth, S. Brewer, F. M. Chambers, J. A. Christen, A. Gallego-Sala, S. P. Harrison, P. D. M. Hughes, S. T. Jackson, A. Korhola, D. Mauquoy, F. J. G. Mitchell, I. C. Prentice, M. van der Linden, F. De Vleeschouwer, Z. C. Yu, J. Alm, I. E. Bauer, Y. M. C. Corish, M. Garneau, V. Hohl, Y. Huang, E. Karofeld, G. Le Roux, J. Loisel, R. Moschen, J. E. Nichols, T. M. Nieminen, G. M. MacDonald, N. R. Phadtare, N. Rausch, Ü. Sillasoo, G. T. Swindles, E.-S. Tuittila, L. Ukonmaanaho, M. Väliranta, S. van Bellen, B. van Geel, D. H. Vitt, and Y. Zhao
Biogeosciences, 10, 929–944, https://doi.org/10.5194/bg-10-929-2013, https://doi.org/10.5194/bg-10-929-2013, 2013
B. Van Bocxlaer, W. Salenbien, N. Praet, and J. Verniers
Biogeosciences, 9, 4497–4512, https://doi.org/10.5194/bg-9-4497-2012, https://doi.org/10.5194/bg-9-4497-2012, 2012
D. Hippler, N. Hu, M. Steiner, G. Scholtz, and G. Franz
Biogeosciences, 9, 1765–1775, https://doi.org/10.5194/bg-9-1765-2012, https://doi.org/10.5194/bg-9-1765-2012, 2012
J. M. Reed, A. Cvetkoska, Z. Levkov, H. Vogel, and B. Wagner
Biogeosciences, 7, 3083–3094, https://doi.org/10.5194/bg-7-3083-2010, https://doi.org/10.5194/bg-7-3083-2010, 2010
Cited articles
Albert, J. S., Carnaval, A. C., Flantua, S. G. A., Lohmann, L. G., Ribas, C. C., Riff, D., Carrillo, J. D., Fan, Y., Figueiredo, J. J. P., Guayasamin, J. M., Hoorn, C., De Melo, G. H., Nascimento, N., Quesada, C. A., Ulloa Ulloa, C., Val, P., Arieira, J., Encalada, A. C., and Nobre, C. A.: Human impacts outpace natural processes in the Amazon, Science, 379, eabo5003, https://doi.org/10.1126/science.abo5003, 2023.
Ammann, B., Birks, H. J. B., Brooks, S. J., Eicher, U., von Grafenstein, U., Hofmann, W., Lemdahl, G., Schwander, J., Tobolski, K., and Wick, L.: Quantification of biotic responses to rapid climatic changes around the Younger Dryas – a synthesis, Palaeogeogr. Palaeocl., 159, 313–347, 2000.
Bennett, K. D. and Humphry, R. W.: Analysis of late-glacial and Holocene rates of vegetational change at two sites in the British Isles, Rev. Palaeobot. Palynol., 85, 263–287, 1995.
Bennion, H., Battarbee, R. W., Sayer, C. D., Simpson, G. L., and Davidson, T. A.: Defining reference conditions and restoration targets for lake ecosystems using palaeolimnology: a synthesis, J. Paleolimnol., 45, 533–544, 2011.
Bigler, C., Von Gunten, L., Lotter, A. F., Hausmann, S., Blass, A., Ohlendorf, C., and Sturm, M.: Quantifying human-induced eutrophication in Swiss mountain lakes since AD 1800 using diatoms, Holocene, 17, 1141–1154, https://doi.org/10.1177/0959683607082555, 2007.
Birks, H. J. B.: Contributions of Quaternary botany to modern ecology and biogeography, Plant Ecol. Divers., 12, 189–385, https://doi.org/10.1080/17550874.2019.1646831, 2019.
Birks, H. J. B. and Tinner, W.: Past forests of Europe, in: European Atlas of Forest Tree Species, edited by: San-Miguel-Ayanz, J., de Rigo, D., Caudullo, G., Houston Durrant, T., and Mauri, A., Publications Office of the European Union, Luxembourg, e010c45+, https://doi.org/10.2760/776635, 2016.
Brugger, S. O., Schwikowski, M., Gobet, E., Schwörer, C., Rohr, C., Sigl, M., Henne, S., Pfister, C., Jenk, T. M., Henne, P. D., and Tinner, W.: Alpine Glacier Reveals Ecosystem Impacts of Europe's Prosperity and Peril Over the Last Millennium, Geophys. Res. Lett., 48, e2021GL095039, https://doi.org/10.1029/2021GL095039, 2021.
Burge, O. R., Richardson, S. J., Wood, J. R., and Wilmshurst, J. M.: A guide to assess distance from ecological baselines and change over time in palaeoecological records, Holocene, 33, 09596836231169986, https://doi.org/10.1177/09596836231169986, 2023.
Clewell, A. F. and Aronson, J.: Ecological restoration: principles, values, and structure of an emerging profession, 2nd ed., Island Press, Washington DC, 303 pp., https://doi.org/10.5822/978-1-59726-323-8, 2013.
Edrisi, S. A. and Abhilash, P. C.: Need of transdisciplinary research for accelerating land restoration during the UN Decade on Ecosystem Restoration, Restor. Ecol., 29, e13531, https://doi.org/10.1111/rec.13531, 2021.
Finsinger, W.: paleo_perc_change (v1.0.1), Zenodo [code], https://doi.org/10.5281/zenodo.10630763, 2024.
Finsinger, W. and Tinner, W.: Holocene vegetation and land-use changes in the forelands of the southwestern Alps, Italy, J. Quat. Sci., 21, 243–258, 2006.
Finsinger, W., Bigler, C., Krähenbühl, U., Lotter, A. F., and Ammann, B.: Human impact and eutrophication patterns during the past ∼ 200 yrs at Lago Grande di Avigliana (N. Italy), J. Paleolimnol., 36, 55–67, 2006.
Finsinger, W., Giesecke, T., Brewer, S., and Leydet, M.: Emergence patterns of novelty in European vegetation assemblages over the past 15 000 years, Ecol. Lett., 20, 336–346, https://doi.org/10.1111/ele.12731, 2017.
Finsinger, W., Bigler, C., Krähenbühl, U., Lotter, A. F., and Ammann, B.: Lago Grande di Avigliana pollen dataset, Neotoma Paleoecological Database [data set], https://doi.org/10.21233/CD0E-0190, 2019.
Fuchs, R., Herold, M., Verburg, P. H., and Clevers, J. G. P. W.: A high-resolution and harmonized model approach for reconstructing and analysing historic land changes in Europe, Biogeosciences, 10, 1543–1559, https://doi.org/10.5194/bg-10-1543-2013, 2013.
Giesecke, T., Davis, B., Brewer, S., Finsinger, W., Wolters, S., Blaauw, M., De Beaulieu, J.-L., Binney, H., Fyfe, R. M., Gaillard, M.-J., Gil-Romera, G., Knaap, W. O., Kuneš, P., Kühl, N., Leeuwen, J. F. N., Leydet, M., Lotter, A. F., Ortu, E., Semmler, M., and Bradshaw, R. H. W.: Towards mapping the late Quaternary vegetation change of Europe, Veg. Hist. Archaeobotany, 23, 75–86, https://doi.org/10.1007/s00334-012-0390-y, 2014.
Gillson, L.: Paleoecology reveals lost ecological connections and strengthens ecosystem restoration, P. Natl. Acad. Sci. USA, 119, e2206436119, https://doi.org/10.1073/pnas.2206436119, 2022.
IPBES: Summary for policymakers of the global assessment report on biodiversity and ecosystem services of the Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services, edited by: Díaz, S., Settele, J., Brondízio, E. S., Ngo, H. T., Guèze, M., Agard, J., Arneth, A., Balvanera, P., Brauman, K. A., Butchart, S. H. M., Chan, K. M. A., Garibaldi, L. A., Ichii, K., Liu, J., Subramanian, S. M., Midgley, G. F., Miloslavich, P., Molnár, Z., Obura, D., Pfaff, A., Polasky, S., Purvis, A., Razzaque, J., Reyers, B., Roy Chowdhury, R., Shin, Y. J., Visseren-Hamakers, I. J., Willis, K. J., and Zayas, C. N., IPBES Secretariat, Bonn, Germany, ISBN 978-3-947851-13-3, 2019.
Jackson, S. T. and Hobbs, R. J.: Ecological restoration in the light of ecological history, Science, 325, 567–569, https://doi.org/10.1126/science.1172977, 2009.
Jacobson, G. L. and Grimm, E. C.: A Numerical Analysis of Holocene Forest and Prairie Vegetation in Central Minnesota, Ecology, 67, 958–966, https://doi.org/10.2307/1939818, 1986.
Jouffray, J.-B., Blasiak, R., Norström, A. V., Österblom, H., and Nyström, M.: The Blue Acceleration: The Trajectory of Human Expansion into the Ocean, One Earth, 2, 43–54, https://doi.org/10.1016/j.oneear.2019.12.016, 2020.
Lang, G., Ammann, B., Behre, K.-E., and Tinner, W. (Eds.): Quaternary Vegetation Dynamics of Europe, Haupt Verlag, ISBN 978-3-258-08214-1, 2023.
Lotter, A. F.: The recent eutrophication of Baldeggersee (Switzerland) as assessed by fossil diatom assemblages, Holocene, 8, 395–405, https://doi.org/10.1191/095968398674589725, 1998.
Lotter, A. F., Ammann, B., and Sturm, M.: Rates of change and chronological problems during the late-glacial period, Clim. Dyn., 6, 233–239, 1992.
Lotter, A. F., Birks, H. J. B., Hofmann, W., and Marchetto, A.: Modern diatom, cladocera, chironomid and chrysophyte cyst assemblages as quantitative indicators for the reconstructions of past environmental conditions in the Alps, I. Climate, J. Paleolimnol., 18, 395–420, 1997.
Lyell, C.: Principles of Geology or, the modern changes of the earth and its inhabitants considered as illustrative of Geology, D. Appleton & Co., New York, 1854.
Manzano, S., Julier, A. C. M., Dirk, C. J., Razafimanantsoa, A. H. I., Samuels, I., Petersen, H., Gell, P., Hoffman, M. T., and Gillson, L.: Using the past to manage the future: the role of palaeoecological and long-term data in ecological restoration, Restor. Ecol., 28, 1335–1342, https://doi.org/10.1111/rec.13285, 2020.
Marchetto, A., Lami, A., Musazzi, S., Massaferro, J., Langone, L., and Guilizzoni, P.: Lake Maggiore (N. Italy) trophic history: fossil diatom, plant pigments, and chironomids, and comparison with long-term limnological data, Quaternary Int., 113, 97–110, https://doi.org/10.1016/S1040-6182(03)00082-X, 2004.
Mottl, O., Flantua, S. G. A., Bhatta, K. P., Felde, V. A., Giesecke, T., Goring, S., Grimm, E. C., Haberle, S., Hooghiemstra, H., Ivory, S., Kuneš, P., Wolters, S., Seddon, A. W. R., and Williams, J. W.: Global acceleration in rates of vegetation change over the past 18,000 years, Science, 372, 860–864, https://doi.org/10.1126/science.abg1685, 2021a.
Mottl, O., Grytnes, J.-A., Seddon, A. W. R., Steinbauer, M. J., Bhatta, K. P., Felde, V. A., Flantua, S. G. A., and Birks, H. J. B.: Rate-of-change analysis in paleoecology revisited: A new approach, Rev. Palaeobot. Palynol., 293, 104483, https://doi.org/10.1016/j.revpalbo.2021.104483, 2021b.
Nogué, S., Santos, A. M. C., Birks, H. J. B., Björck, S., Castilla-Beltrán, A., Connor, S., De Boer, E. J., De Nascimento, L., Felde, V. A., Fernández-Palacios, J. M., Froyd, C. A., Haberle, S. G., Hooghiemstra, H., Ljung, K., Norder, S. J., Peñuelas, J., Prebble, M., Stevenson, J., Whittaker, R. J., Willis, K. J., Wilmshurst, J. M., and Steinbauer, M. J.: The human dimension of biodiversity changes on islands, Science, 372, 488–491, https://doi.org/10.1126/science.abd6706, 2021.
Nogué, S., De Nascimento, L., Gosling, W. D., Loughlin, N. J. D., Montoya, E., and Wilmshurst, J. M.: Multiple baselines for restoration ecology, Past Glob. Change Mag., 30, 4–5, https://doi.org/10.22498/pages.30.1.4, 2022.
Overpeck, J. T. and Breshears, D. D.: The growing challenge of vegetation change, Science, 372, 786–787, https://doi.org/10.1126/science.abi9902, 2021.
Pereira, H. M., Ferrier, S., Walters, M., Geller, G. N., Jongman, R. H. G., Scholes, R. J., Bruford, M. W., Brummitt, N., Butchart, S. H. M., Cardoso, A. C., Coops, N. C., Dulloo, E., Faith, D. P., Freyhof, J., Gregory, R. D., Heip, C., Höft, R., Hurtt, G., Jetz, W., Karp, D. S., McGeoch, M. A., Obura, D., Onoda, Y., Pettorelli, N., Reyers, B., Sayre, R., Scharlemann, J. P. W., Stuart, S. N., Turak, E., Walpole, M., and Wegmann, M.: Essential Biodiversity Variables, Science, 339, 277–278, https://doi.org/10.1126/science.1229931, 2013.
Purvis, A., Molnár, Z., Obura, D., Ichii, K., Willis, K., Chettri, N., Dulloo, M., Hendry, A., Gabrielyan, B., Gutt, J., Jacob, U., Keskin, E., Niamir, A., Öztürk, B., Salimov, R., and Jaureguiberry, P.: Status and Trends – Nature, Chap. 2.2, in: Global assessment report of the Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services, edited by: Brondizio, E. S., Settele, J., Díaz, S., and Ngo, H. T., IPBES secretariat, Bonn, Germany, 108, https://doi.org/10.5281/zenodo.3831674, 2019.
R Core Team: R: A language and environment for statistical computing, R Foundation for Statistical Computing, Vienna, Austria, https://www.R-project.org/ (last access: 2 April 2024), 2022.
Rey, F., Gobet, E., Schwörer, C., Wey, O., Hafner, A., and Tinner, W.: Causes and mechanisms of synchronous succession trajectories in primeval Central European mixed Fagus sylvatica forests, J. Ecol., 107, 1392–1408, https://doi.org/10.1111/1365-2745.13121, 2019.
Schibler, J., Jacomet, S., Hüster-Plogmann, H., and Brombacher, C.: Economic crash in the 37th and 36th centuries cal. BC in Neolithic lake shore sites in Switzerland, Anthropozoologica, 25–26, 553–570, 1997.
Seddon, A. W., Macias-Fauria, M., and Willis, K. J.: Climate and abrupt vegetation change in Northern Europe since the last deglaciation, The Holocene, 25, 25–36, 2015.
Seppä, H.: Pollen Analysis, Principles, in: Encyclopedia of Quaternary Science, Elsevier, 794–804, https://doi.org/10.1016/B978-0-444-53643-3.00171-0, 2013.
Smol, J. P.: Pollution of lakes and rivers: a paleoenvironmental perspective, Wiley-Blackwell, ISBN: 978-1-405-15913-5, 2008.
Steffen, W., Broadgate, W., Deutsch, L., Gaffney, O., and Ludwig, C.: The trajectory of the Anthropocene: The Great Acceleration, Anthr. Rev., 2, 81–98, https://doi.org/10.1177/2053019614564785, 2015.
Sugita, S.: Pollen representation of vegetation in Quaternary sediments – theory and method in patchy vegetation, J. Ecol., 82, 881–897, 1994.
Tinner, W.: Long-term disturbance ecology, in: Quaternary Vegetation Dynamics of Europe, edited by: Lang, G., Ammann, B., Behre, K.-E., and Tinner, W., Haupt Verlag, 467–485, ISBN 978-3-258-08214-1, 2023.
Tinner, W., Conedera, M., Ammann, B., Gaggeler, H. W., Gedye, S., Jones, R., and Sagesser, B.: Pollen and charcoal in lake sediments compared with historically documented forest fires in southern Switzerland since AD 1920, Holocene, 8, 31–42, 1998.
Tinner, W., Lotter, A. F., Ammann, B., Conedera, M., Hubschmid, P., van Leeuwen, J. F. N., and Wehrli, M.: Climatic change and contemporaneous land-use phases north and south of the Alps 2300 BC to 800 AD, Quaternary Sci. Rev., 22, 1447–1460, 2003.
van der Knaap, W. O., van Leeuwen, J. F. N., Fankhauser, A., and Ammann, B.: Palynostratigraphy of the last centuries in Switzerland based on 23 lake and mire deposits: chronostratigraphic pollen markers, regional patterns, and local histories, Rev. Paleaobot. Palynol., 108, 85–142, 2000.
Veldman, J. W., Aleman, J. C., Alvarado, S. T., Anderson, T. M., Archibald, S., Bond, W. J., Boutton, T. W., Buchmann, N., Buisson, E., Canadell, J. G., Dechoum, M. D. S., Diaz-Toribio, M. H., Durigan, G., Ewel, J. J., Fernandes, G. W., Fidelis, A., Fleischman, F., Good, S. P., Griffith, D. M., Hermann, J.-M., Hoffmann, W. A., Le Stradic, S., Lehmann, C. E. R., Mahy, G., Nerlekar, A. N., Nippert, J. B., Noss, R. F., Osborne, C. P., Overbeck, G. E., Parr, C. L., Pausas, J. G., Pennington, R. T., Perring, M. P., Putz, F. E., Ratnam, J., Sankaran, M., Schmidt, I. B., Schmitt, C. B., Silveira, F. A. O., Staver, A. C., Stevens, N., Still, C. J., Strömberg, C. A. E., Temperton, V. M., Varner, J. M., and Zaloumis, N. P.: Comment on “The global tree restoration potential”, Science, 366, eaay7976, https://doi.org/10.1126/science.aay7976, 2019.
Whitlock, C., Colombaroli, D., Conedera, M., and Tinner, W.: Land-use history as a guide for forest conservation and management, Conserv. Biol., 32, 84–97, https://doi.org/10.1111/cobi.12960, 2018.
Williams, J. W., Grimm, E. C., Blois, J. L., Charles, D. F., Davis, E. B., Goring, S. J., Graham, R. W., Smith, A. J., Anderson, M., Arroyo-Cabrales, J., Ashworth, A. C., Betancourt, J. L., Bills, B. W., Booth, R. K., Buckland, P. I., Curry, B. B., Giesecke, T., Jackson, S. T., Latorre, C., Nichols, J., Purdum, T., Roth, R. E., Stryker, M., and Takahara, H.: The Neotoma Paleoecology Database, a multiproxy, international, community-curated data resource, Quaternary Res., 89, 156–177, https://doi.org/10.1017/qua.2017.105, 2018.
Williams, J. W., Ordonez, A., and Svenning, J.-C.: A unifying framework for studying and managing climate-driven rates of ecological change, Nat. Ecol. Evol., 5, 17–26, https://doi.org/10.1038/s41559-020-01344-5, 2021.
Willis, K. J., Bailey, R. M., Bhagwat, S. A., and Birks, H. J. B.: Biodiversity baselines, thresholds and resilience: testing predictions and assumptions using palaeoecological data, Trends Ecol. Evol., 25, 583–591, https://doi.org/10.1016/j.tree.2010.07.006, 2010.
Co-editor-in-chief
Ecosystems are, in many ways, changing more rapidly than they have in the past. Rapid past ecological changes can provide critical insight into how to best understand ecosystem function to improve ecological restoration, but a historic focus on community composition in the paleoecological literature can obscure the causes of these changes, making mechanisms unclear. The authors demonstrate a path forward using pollen and diatom records from a lake in the Italian Alps to construct a narrative of terrestrial and aquatic ecosystem changes that combines well-established vegetation changes with rapid changes to water management changes to explore how rapidly the ecosystem responds to perturbations, and how aquatic function has been restored after pollution events. Doing so provides new insight into how to use the paleoecological record to understand restoration success and the time scales upon which ecosystem changes occur.
Ecosystems are, in many ways, changing more rapidly than they have in the past. Rapid past...
Short summary
Rate-of-change records based on compositional data are ambiguous as they may rise irrespective of the underlying trajectory of ecosystems. We emphasize the importance of characterizing both the direction and the rate of palaeoecological changes in terms of key features of ecosystems rather than solely on community composition. Past accelerations of community transformation may document the potential of ecosystems to rapidly recover important ecological attributes and functions.
Rate-of-change records based on compositional data are ambiguous as they may rise irrespective...
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