Holocene vegetation change and turnovers of treeline forming species

The prospected strong high-latitude warming is projected to cause a northward move of the arctic-boreal treeline. These changes will potentially have significant effects on climate, but their timing and mode are not well understood. Besides being governed directly by temperature increases, speed of...

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Main Authors: Epp, Laura Saskia, Kruse, Stefan, Kath, Nadja, Pestryakova, Luidmila, Herzschuh, Ulrike
Format: Conference Object
Language:unknown
Published: 2016
Subjects:
Online Access:https://epic.awi.de/id/eprint/41332/
https://epic.awi.de/id/eprint/41332/1/Poster_ICOP_Epp.pdf
https://hdl.handle.net/10013/epic.48378
https://hdl.handle.net/10013/epic.48378.d001
id ftawi:oai:epic.awi.de:41332
record_format openpolar
spelling ftawi:oai:epic.awi.de:41332 2024-09-15T18:30:00+00:00 Holocene vegetation change and turnovers of treeline forming species Epp, Laura Saskia Kruse, Stefan Kath, Nadja Pestryakova, Luidmila Herzschuh, Ulrike 2016-06-23 application/pdf https://epic.awi.de/id/eprint/41332/ https://epic.awi.de/id/eprint/41332/1/Poster_ICOP_Epp.pdf https://hdl.handle.net/10013/epic.48378 https://hdl.handle.net/10013/epic.48378.d001 unknown https://epic.awi.de/id/eprint/41332/1/Poster_ICOP_Epp.pdf https://hdl.handle.net/10013/epic.48378.d001 Epp, L. S. , Kruse, S. orcid:0000-0003-1107-1958 , Kath, N. , Pestryakova, L. and Herzschuh, U. orcid:0000-0003-0999-1261 (2016) Holocene vegetation change and turnovers of treeline forming species , XI. International Conference on Permafrost, 20 June 2016 - 24 June 2016 . hdl:10013/epic.48378 EPIC3XI. International Conference on Permafrost, 2016-06-20-2016-06-24 Conference notRev 2016 ftawi 2024-06-24T04:14:20Z The prospected strong high-latitude warming is projected to cause a northward move of the arctic-boreal treeline. These changes will potentially have significant effects on climate, but their timing and mode are not well understood. Besides being governed directly by temperature increases, speed of treeline changes will also be influenced by the capacity of migration and establishment, and by competition between different treeline forming species. In Siberia, where about half of the global circum-arctic boreal treeline is located, the treeline is formed by monospecific stands of three species of larch, Larix sibirica, Larix gmelinii and Larix cajanderi. There is clear evidence for ecological separation, particularly between L. sibirica and the northeastern species, with only L. gmelinii and L. cajanderi being able to survive on permafrost with an active layer depth of less than 1-2 m, but L. sibirica being competitively superior at sites with low permafrost tables. Under a warming climate, the respective ranges of the treeline forming species are projected to shift to the Northeast, causing turnovers of forest tree species. The Siberian treeline has undergone several pronounced latitudinal fluctuations in the Holocene, and detailed analyses of the historical processes of vegetation change and competitive displacement would add to predictions for the projected future shift. We are using sedimentary ancient DNA to analyze lake sediment cores spanning most of the Holocene from the southern Taymyr peninsula, where the ranges of L. sibirica and L. gmelinii come together. Changes of the complete vegetation are revealed by DNA metabarcoding and pollen analyses, while diagnostic mitochondrial haplotypes trace the temporal dynamics in distribution of the two closely related larch species. We incorporated these two species into our larch population dynamics model LAVESI to understand the influence competition between these species might have on the speed and timing of treeline movement under changing climates. Simulations ... Conference Object permafrost Taymyr Taymyr Peninsula Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description The prospected strong high-latitude warming is projected to cause a northward move of the arctic-boreal treeline. These changes will potentially have significant effects on climate, but their timing and mode are not well understood. Besides being governed directly by temperature increases, speed of treeline changes will also be influenced by the capacity of migration and establishment, and by competition between different treeline forming species. In Siberia, where about half of the global circum-arctic boreal treeline is located, the treeline is formed by monospecific stands of three species of larch, Larix sibirica, Larix gmelinii and Larix cajanderi. There is clear evidence for ecological separation, particularly between L. sibirica and the northeastern species, with only L. gmelinii and L. cajanderi being able to survive on permafrost with an active layer depth of less than 1-2 m, but L. sibirica being competitively superior at sites with low permafrost tables. Under a warming climate, the respective ranges of the treeline forming species are projected to shift to the Northeast, causing turnovers of forest tree species. The Siberian treeline has undergone several pronounced latitudinal fluctuations in the Holocene, and detailed analyses of the historical processes of vegetation change and competitive displacement would add to predictions for the projected future shift. We are using sedimentary ancient DNA to analyze lake sediment cores spanning most of the Holocene from the southern Taymyr peninsula, where the ranges of L. sibirica and L. gmelinii come together. Changes of the complete vegetation are revealed by DNA metabarcoding and pollen analyses, while diagnostic mitochondrial haplotypes trace the temporal dynamics in distribution of the two closely related larch species. We incorporated these two species into our larch population dynamics model LAVESI to understand the influence competition between these species might have on the speed and timing of treeline movement under changing climates. Simulations ...
format Conference Object
author Epp, Laura Saskia
Kruse, Stefan
Kath, Nadja
Pestryakova, Luidmila
Herzschuh, Ulrike
spellingShingle Epp, Laura Saskia
Kruse, Stefan
Kath, Nadja
Pestryakova, Luidmila
Herzschuh, Ulrike
Holocene vegetation change and turnovers of treeline forming species
author_facet Epp, Laura Saskia
Kruse, Stefan
Kath, Nadja
Pestryakova, Luidmila
Herzschuh, Ulrike
author_sort Epp, Laura Saskia
title Holocene vegetation change and turnovers of treeline forming species
title_short Holocene vegetation change and turnovers of treeline forming species
title_full Holocene vegetation change and turnovers of treeline forming species
title_fullStr Holocene vegetation change and turnovers of treeline forming species
title_full_unstemmed Holocene vegetation change and turnovers of treeline forming species
title_sort holocene vegetation change and turnovers of treeline forming species
publishDate 2016
url https://epic.awi.de/id/eprint/41332/
https://epic.awi.de/id/eprint/41332/1/Poster_ICOP_Epp.pdf
https://hdl.handle.net/10013/epic.48378
https://hdl.handle.net/10013/epic.48378.d001
genre permafrost
Taymyr
Taymyr Peninsula
Siberia
genre_facet permafrost
Taymyr
Taymyr Peninsula
Siberia
op_source EPIC3XI. International Conference on Permafrost, 2016-06-20-2016-06-24
op_relation https://epic.awi.de/id/eprint/41332/1/Poster_ICOP_Epp.pdf
https://hdl.handle.net/10013/epic.48378.d001
Epp, L. S. , Kruse, S. orcid:0000-0003-1107-1958 , Kath, N. , Pestryakova, L. and Herzschuh, U. orcid:0000-0003-0999-1261 (2016) Holocene vegetation change and turnovers of treeline forming species , XI. International Conference on Permafrost, 20 June 2016 - 24 June 2016 . hdl:10013/epic.48378
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