Data from: The history of tree and shrub taxa on Bol'shoy Lyakhovsky Island (New Siberian Archipelago) since the last interglacial uncovered by sedimentary ancient DNA and pollen data ...
Ecosystem boundaries, such as the Arctic-Boreal treeline, are strongly coupled with climate and were spatially highly dynamic during past glacial-interglacial cycles. Only a few studies cover vegetation changes since the last interglacial, as most of the former landscapes are inundated and difficult...
| Main Authors: | , , , , , , |
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| Format: | Dataset |
| Language: | English |
| Published: |
Dryad
2020
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.5061/dryad.866t1g1p5 https://datadryad.org/stash/dataset/doi:10.5061/dryad.866t1g1p5 |
| Summary: | Ecosystem boundaries, such as the Arctic-Boreal treeline, are strongly coupled with climate and were spatially highly dynamic during past glacial-interglacial cycles. Only a few studies cover vegetation changes since the last interglacial, as most of the former landscapes are inundated and difficult to access. Using pollen analysis and sedimentary ancient DNA (sedaDNA) metabarcoding, we reveal vegetation changes on Bol’shoy Lyakhovsky Island since the last interglacial from permafrost sediments. Last interglacial samples depict high levels of floral diversity with the presence of trees (Larix, Picea, Populus) and shrubs (Alnus, Betula, Ribes, Cornus, Saliceae) on the currently treeless island. After the Last Glacial Maximum, Larix re-colonised the island but disappeared along with most shrub taxa. This was probably caused by Holocene sea-level rise, which led to increased oceanic conditions on the island. Additionally, we applied two newly developed larch-specific chloroplast markers to evaluate their ... : In this study we analysed plant-derived sedimentary ancient DNA (sedaDNA) from permafrost cores L14-2, L14-3, L14-4 and L14-5 to investigate past vegetation change on Bol’shoy Lyakhovsky Island. A core barrel loss in the borehole prevented further drilling and four additional samples (hand-pieces) L14-04B were collected from the coastal bluff from layers resembling the upper part of core L14-04 while five additional samples L14-04C originated from ice-wedge casts resembling the lower part of the core. Total DNA was extracted from 72 samples and 8 negative controls. The PCR reactions were performed with the trnL g and h primers (Taberlet et al., 2007). Both primers were modified on the 5′end by unique 8 bp tags which varied from each other in at least five base pairs to distinguish samples after sequencing (Binladen et al., 2007) and were additionally elongated by NNN tagging to improve cluster detection on the sequencing platform (De Barba etal., 2014). For each sample, we pooled two positive PCR products ... |
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