Sedimentary ancient DNA and pollen reveal the composition of plant organic matter in Late Quaternary permafrost sediments of the Buor Khaya Peninsula (north-eastern Siberia)
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Zimmermann, Heike Hildegard
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Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Univ Potsdam, Inst Earth & Environm Sci, Karl Liebknecht Str 24-25, D-14476 Potsdam, GermanyAlfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Zimmermann, Heike Hildegard
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Raschke, Elena
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Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Arctic & Antarctic Res Inst, Bering St 38, St Petersburg 199397, RussiaAlfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Raschke, Elena
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Epp, Laura Saskia
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Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, GermanyAlfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Epp, Laura Saskia
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Stoof-Leichsenring, Kathleen Rosmarie
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Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, GermanyAlfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Stoof-Leichsenring, Kathleen Rosmarie
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Schwamborn, Georg
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Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, GermanyAlfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Schwamborn, Georg
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Schirrmeister, Lutz
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Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, GermanyAlfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Schirrmeister, Lutz
[1
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Overduin, Pier Paul
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Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, GermanyAlfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Overduin, Pier Paul
[1
]
Herzschuh, Ulrike
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Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Univ Potsdam, Inst Earth & Environm Sci, Karl Liebknecht Str 24-25, D-14476 Potsdam, GermanyAlfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Herzschuh, Ulrike
[1
,2
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机构:
[1] Alfred Wegener Inst Helmholtz Ctr Polar & Marine, Periglacial Res Unit, Telegrafenberg A43, D-14473 Potsdam, Germany
Organic matter deposited in ancient, ice-rich permafrost sediments is vulnerable to climate change and may contribute to the future release of greenhouse gases; it is thus important to get a better characterization of the plant organic matter within such sediments. From a Late Quaternary permafrost sediment core from the Buor Khaya Peninsula, we analysed plant-derived sedimentary ancient DNA (sedaDNA) to identify the taxonomic composition of plant organic matter, and undertook palynological analysis to assess the environmental conditions during deposition. Using sedaDNA, we identified 154 taxa and from pollen and non-pollen palynomorphs we identified 83 taxa. In the deposits dated between 54 and 51 kyr BP, sedaDNA records a diverse low-centred polygon plant community including recurring aquatic pond vegetation while from the pollen record we infer terrestrial open-land vegetation with relatively dry environmental conditions at a regional scale. A fluctuating dominance of either terrestrial or swamp and aquatic taxa in both proxies allowed the local hydrological development of the polygon to be traced. In deposits dated between 11.4 and 9.7 kyr BP (13.4-11.1 cal kyr BP), sedaDNA shows a taxonomic turnover to moist shrub tundra and a lower taxonomic richness compared to the older samples. Pollen also records a shrub tundra community, mostly seen as changes in relative proportions of the most dominant taxa, while a decrease in taxonomic richness was less pronounced compared to sedaDNA. Our results show the advantages of using sedaDNA in combination with palynological analyses when macrofossils are rarely preserved. The high resolution of the sedaDNA record provides a detailed picture of the taxonomic composition of plant-derived organic matter throughout the core, and palynological analyses prove valuable by allowing for inferences of regional environmental conditions.