Articles | Volume 13, issue 4
https://doi.org/10.5194/bg-13-1351-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-1351-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
03 Mar 2016
Research article |
| 03 Mar 2016
Complexity of diatom response to Lateglacial and Holocene climate and environmental change in ancient, deep and oligotrophic Lake Ohrid (Macedonia and Albania)
X. S. Zhang
CORRESPONDING AUTHOR
Institute of Loess Plateau, Shanxi University, Taiyuan, China
Department of Geography, Environment and Earth Sciences, University of
Hull, Hull, UK
J. M. Reed
Department of Geography, Environment and Earth Sciences, University of
Hull, Hull, UK
J. H. Lacey
Centre for Environmental Geochemistry, School of Geography, University
of Nottingham, Nottingham, UK
NERC Isotope Geosciences Facilities, British Geological Survey,
Nottingham, UK
A. Francke
Institute of Geology and Mineralogy, University of Cologne, Cologne,
Germany
M. J. Leng
Centre for Environmental Geochemistry, School of Geography, University
of Nottingham, Nottingham, UK
NERC Isotope Geosciences Facilities, British Geological Survey,
Nottingham, UK
Z. Levkov
Institute of Biology, Faculty of Natural Sciences, Ss. Cyril and
Methodius University, Skopje, Republic of Macedonia
B. Wagner
Institute of Geology and Mineralogy, University of Cologne, Cologne,
Germany
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M. Damaschke, R. Sulpizio, G. Zanchetta, B. Wagner, A. Böhm, N. Nowaczyk, J. Rethemeyer, and A. Hilgers
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Clim. Past, 9, 135–148, https://doi.org/10.5194/cp-9-135-2013, https://doi.org/10.5194/cp-9-135-2013, 2013
B. Wagner, A. Francke, R. Sulpizio, G. Zanchetta, K. Lindhorst, S. Krastel, H. Vogel, J. Rethemeyer, G. Daut, A. Grazhdani, B. Lushaj, and S. Trajanovski
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Our micropaleontological analyses on three cores from New Jersey (USA) show that the late Maastrichtian warming event (66.4–66.1 Ma), characterized by a ~ 4.0 °C warming of sea waters on the New Jersey paleoshelf, resulted in a disruption of phytoplankton communities and a stressed benthic ecosystem. This increased ecosystem stress during the latest Maastrichtian potentially primed global ecosystems for the subsequent mass extinction following the Cretaceous–Paleogene boundary impact.
Baptiste Suchéras-Marx, Emanuela Mattioli, Pascal Allemand, Fabienne Giraud, Bernard Pittet, Julien Plancq, and Gilles Escarguel
Biogeosciences, 16, 2501–2510, https://doi.org/10.5194/bg-16-2501-2019, https://doi.org/10.5194/bg-16-2501-2019, 2019
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Calcareous nannoplankton are photosynthetic plankton producing micrometric calcite platelets having a fossil record covering the past 200 Myr. Based on species richness, platelets size and abundance we observed four evolution phases through time: Jurassic–Early Cretaceous invasion phase of the open ocean, Early Cretaceous–K–Pg extinction specialization phase to the ecological niches, post-K–Pg mass extinction recovery and Eocene–Neogene establishment phase with domination of a few small species.
Sabrina van de Velde, Elisabeth L. Jorissen, Thomas A. Neubauer, Silviu Radan, Ana Bianca Pavel, Marius Stoica, Christiaan G. C. Van Baak, Alberto Martínez Gándara, Luis Popa, Henko de Stigter, Hemmo A. Abels, Wout Krijgsman, and Frank P. Wesselingh
Biogeosciences, 16, 2423–2442, https://doi.org/10.5194/bg-16-2423-2019, https://doi.org/10.5194/bg-16-2423-2019, 2019
Kweku Afrifa Yamoah, Nolwenn Callac, Ernest Chi Fru, Barbara Wohlfarth, Alan Wiech, Akkaneewut Chabangborn, and Rienk H. Smittenberg
Biogeosciences, 13, 3971–3980, https://doi.org/10.5194/bg-13-3971-2016, https://doi.org/10.5194/bg-13-3971-2016, 2016
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Predicting the effects of changing climate on microbial community shifts on longer timescales can be challenging. This study exploits the power of combining organic geochemistry, molecular microbial ecology, and geochemistry to unravel trends in microbial community induced by climatic variability. Our results show that climate-induced variability on decadal timescales can trigger changes in both lake trophic status and phytoplankton communities.
Perran L. M. Cook, Miles Jennings, Daryl P. Holland, John Beardall, Christy Briles, Atun Zawadzki, Phuong Doan, Keely Mills, and Peter Gell
Biogeosciences, 13, 3677–3686, https://doi.org/10.5194/bg-13-3677-2016, https://doi.org/10.5194/bg-13-3677-2016, 2016
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The Gippsland Lakes, Australia, have suffered from periodic blooms of cyanobacteria (blue green algae) since the mid 1980s. Prior to this, little is known about the history of cyanobacterial blooms in this system. We investigated the history of cyanobacterial blooms using a sediment core taken from the Gippsland Lakes which had each layer dated using lead isotopes. The results showed that surprising blooms of cyanobacteria were also prevalent prior to European settlement
Mathias Harzhauser, Ana Djuricic, Oleg Mandic, Thomas A. Neubauer, Martin Zuschin, and Norbert Pfeifer
Biogeosciences, 13, 1223–1235, https://doi.org/10.5194/bg-13-1223-2016, https://doi.org/10.5194/bg-13-1223-2016, 2016
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We present the first analysis of population structure and cohort distribution in a fossil oyster reef. Data are derived from Terrestrial Laser Scanning of a Miocene shell bed covering 459 m². A growth model was calculated, revealing this species as the giant oyster Crassostrea gryphoides was the fastest growing oyster known so far. The shell half-lives range around few years, indicating that oyster reefs were geologically short-lived structures, which were degraded on a decadal scale.
K. Michaelian and A. Simeonov
Biogeosciences, 12, 4913–4937, https://doi.org/10.5194/bg-12-4913-2015, https://doi.org/10.5194/bg-12-4913-2015, 2015
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We show that the fundamental molecules of life (those common to all three domains of life: Archaea, Bacteria, Eukaryota), including nucleotides, amino acids, enzyme cofactors, and porphyrin agglomerates, absorb light strongly from 230 to 280nm (in the UV-C) and have chemical affinity to RNA and DNA. This supports the "thermodynamic dissipation theory for the origin of life", which suggests that life arose and evolved as a response to dissipating the prevailing Archaean UV-C sunlight into heat.
D. Bolshiyanov, A. Makarov, and L. Savelieva
Biogeosciences, 12, 579–593, https://doi.org/10.5194/bg-12-579-2015, https://doi.org/10.5194/bg-12-579-2015, 2015
P. Bragée, F. Mazier, A. B. Nielsen, P. Rosén, D. Fredh, A. Broström, W. Granéli, and D. Hammarlund
Biogeosciences, 12, 307–322, https://doi.org/10.5194/bg-12-307-2015, https://doi.org/10.5194/bg-12-307-2015, 2015
I. Ruvalcaba Baroni, R. P. M. Topper, N. A. G. M. van Helmond, H. Brinkhuis, and C. P. Slomp
Biogeosciences, 11, 977–993, https://doi.org/10.5194/bg-11-977-2014, https://doi.org/10.5194/bg-11-977-2014, 2014
M. Taviani, L. Angeletti, A. Ceregato, F. Foglini, C. Froglia, and F. Trincardi
Biogeosciences, 10, 4653–4671, https://doi.org/10.5194/bg-10-4653-2013, https://doi.org/10.5194/bg-10-4653-2013, 2013
S. J. Gibbs, P. R. Bown, B. H. Murphy, A. Sluijs, K. M. Edgar, H. Pälike, C. T. Bolton, and J. C. Zachos
Biogeosciences, 9, 4679–4688, https://doi.org/10.5194/bg-9-4679-2012, https://doi.org/10.5194/bg-9-4679-2012, 2012
Z. C. Yu
Biogeosciences, 9, 4071–4085, https://doi.org/10.5194/bg-9-4071-2012, https://doi.org/10.5194/bg-9-4071-2012, 2012
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