Articles | Volume 12, issue 2
https://doi.org/10.5194/cp-12-575-2016
© 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/cp-12-575-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Impacts of climate and humans on the vegetation in northwestern Turkey: palynological insights from Lake Iznik since the Last Glacial
Andrea Miebach
CORRESPONDING AUTHOR
Steinmann Institute for Geology, Mineralogy, and
Paleontology, University of Bonn, Bonn, Germany
Invited contribution by A. Miebach, recipient of the EGU Young Scientists Outstanding Poster Paper Award 2015.
Phoebe Niestrath
Steinmann Institute for Geology, Mineralogy, and
Paleontology, University of Bonn, Bonn, Germany
Patricia Roeser
Steinmann Institute for Geology, Mineralogy, and
Paleontology, University of Bonn, Bonn, Germany
Thomas Litt
Steinmann Institute for Geology, Mineralogy, and
Paleontology, University of Bonn, Bonn, Germany
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New probabilistic methods for local quantitative palaeoclimate reconstructions are presented in a Bayesian framework and applied to plant proxy data from Lake Kinneret. We use recent climate data and arboreal pollen from the sediment of this lake as predefined boundary conditions. The result shows a climate reconstruction of the mean December–February temperature and annual precipitation with the corresponding uncertainty ranges during the Holocene in this region.
Nadine Pickarski and Thomas Litt
Clim. Past, 13, 689–710, https://doi.org/10.5194/cp-13-689-2017, https://doi.org/10.5194/cp-13-689-2017, 2017
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We present a new detailed pollen and isotope record from Lake Van (Turkey) spanning the period from 250 to 128 ka. In contrast to SW Europe, all three terrestrial warm intervals at Lake Van are characterized by clear interglacial conditions. The largest forest expansion occurred during MIS 7c instead of MIS 7e. Our record also reveals high oscillations between 193 and 157 ka followed by low variations (157 to 131 ka) that highlighted Dansgaard–Oeschger-like events during the penultimate glacial.
N. Pickarski, O. Kwiecien, D. Langgut, and T. Litt
Clim. Past, 11, 1491–1505, https://doi.org/10.5194/cp-11-1491-2015, https://doi.org/10.5194/cp-11-1491-2015, 2015
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Subject: Vegetation Dynamics | Archive: Terrestrial Archives | Timescale: Millenial/D-O
Relationships between low-temperature fires, climate and vegetation during three late glacials and interglacials of the last 430 kyr in northeastern Siberia reconstructed from monosaccharide anhydrides in Lake El'gygytgyn sediments
A new high-resolution pollen sequence at Lake Van, Turkey: insights into penultimate interglacial–glacial climate change on vegetation history
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Abrupt climate and vegetation variability of eastern Anatolia during the last glacial
Climate variability over the last 92 ka in SW Balkans from analysis of sediments from Lake Prespa
Ultra-high resolution pollen record from the northern Andes reveals rapid shifts in montane climates within the last two glacial cycles
Elisabeth Dietze, Kai Mangelsdorf, Andrei Andreev, Cornelia Karger, Laura T. Schreuder, Ellen C. Hopmans, Oliver Rach, Dirk Sachse, Volker Wennrich, and Ulrike Herzschuh
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Long-term climate change impacts on fire, vegetation and permafrost in the Arctic are uncertain. Here, we show the high potential of organic compounds from low-temperature biomass burning to serve as proxies for surface fires in lake deposits. During warm periods of the last 430 000 years, surface fires are closely linked to the larch taiga forest with its moss–lichen ground vegetation that isolates the permafrost. They have reduced in warm–wet, spruce–dominated and cool–dry steppe environments.
Nadine Pickarski and Thomas Litt
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We present a new detailed pollen and isotope record from Lake Van (Turkey) spanning the period from 250 to 128 ka. In contrast to SW Europe, all three terrestrial warm intervals at Lake Van are characterized by clear interglacial conditions. The largest forest expansion occurred during MIS 7c instead of MIS 7e. Our record also reveals high oscillations between 193 and 157 ka followed by low variations (157 to 131 ka) that highlighted Dansgaard–Oeschger-like events during the penultimate glacial.
Dunia H. Urrego, Henry Hooghiemstra, Oscar Rama-Corredor, Belen Martrat, Joan O. Grimalt, Lonnie Thompson, Mark B. Bush, Zaire González-Carranza, Jennifer Hanselman, Bryan Valencia, and César Velásquez-Ruiz
Clim. Past, 12, 697–711, https://doi.org/10.5194/cp-12-697-2016, https://doi.org/10.5194/cp-12-697-2016, 2016
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We compare eight pollen records reflecting environmental change in the tropical Andes over the past 30 000 years. Our analysis focuses on the signature of millennial-scale climate variability in the tropical Andes: Heinrich stadials (HS) and Greenland interstadials (GI). We identify rapid responses of the tropical vegetation, with downslope upper forest line (UFL) migrations and cooling during HS and the Younger Dryas.
S. G. A. Flantua, M. Blaauw, and H. Hooghiemstra
Clim. Past, 12, 387–414, https://doi.org/10.5194/cp-12-387-2016, https://doi.org/10.5194/cp-12-387-2016, 2016
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We present a review of chronological dating from ca. 1100 fossil pollen records in Central and South America. Additionally, a temporal quality assessment is implemented on 292 records from northwest South America, which include recalibrating 234 age models. This method evaluates uncertainties for inferred sample ages and chronologies. Important time windows on centennial-millennial climate variability are discussed for sample resolution (estimated years/sample) and temporal uncertainty.
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Clim. Past, 11, 1491–1505, https://doi.org/10.5194/cp-11-1491-2015, https://doi.org/10.5194/cp-11-1491-2015, 2015
K. Panagiotopoulos, A. Böhm, M. J. Leng, B. Wagner, and F. Schäbitz
Clim. Past, 10, 643–660, https://doi.org/10.5194/cp-10-643-2014, https://doi.org/10.5194/cp-10-643-2014, 2014
M. H. M. Groot, R. G. Bogotá, L. J. Lourens, H. Hooghiemstra, M. Vriend, J. C. Berrio, E. Tuenter, J. Van der Plicht, B. Van Geel, M. Ziegler, S. L. Weber, A. Betancourt, L. Contreras, S. Gaviria, C. Giraldo, N. González, J. H. F. Jansen, M. Konert, D. Ortega, O. Rangel, G. Sarmiento, J. Vandenberghe, T. Van der Hammen, M. Van der Linden, and W. Westerhoff
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Short summary
We analyze the vegetation and climate in northwestern Turkey during the last ca. 31 000 years based on a new pollen data set from lacustrine sediment cores. The study reveals vegetation responses to long-term and rapid climate changes. Moreover, it documents human activities in the catchment of Lake Iznik and shows a clear anthropogenic impact on the vegetation since the Early Bronze Age.
We analyze the vegetation and climate in northwestern Turkey during the last ca. 31 000 years...