Ancient DNA and osteological analyses of a unique paleo-archive reveal Early Holocene faunal expansion into the Scandinavian Arctic

Author:

Boilard Aurélie1ORCID,Walker Samuel J.1ORCID,Lødøen Trond Klungseth2ORCID,Henriksen Mona3ORCID,Takken Beijersbergen Liselotte M.4ORCID,Star Bastiaan1ORCID,Robu Marius15ORCID,Tøssebro Christine2,Albrektsen Cornelia Marie2,Soleng Yvonne2ORCID,Aksnes Sverre6ORCID,Jørgensen Roger7ORCID,Hufthammer Anne Karin4ORCID,van Kolfschoten Thijs89ORCID,Lauritzen Stein-Erik161011ORCID,Boessenkool Sanne1ORCID

Affiliation:

1. Centre for Ecological and Evolutionary Synthesis (CEES), Department of Biosciences, University of Oslo, Oslo, Norway.

2. Department of Cultural History, University Museum of Bergen, University of Bergen, Bergen, Norway.

3. Faculty of Environmental Sciences and Natural Resource Management, Norwegian University of Life Sciences, Ås, Norway.

4. Department of Natural History, University Museum of Bergen, University of Bergen, Bergen, Norway.

5. Department of Karstonomy, Karst Inventory and Protection, Emil Racoviţă Institute of Speleology, Bucharest, Romania.

6. Department of Earth Sciences, University of Bergen, Bergen, Norway.

7. The Arctic University Museum of Norway, University of Tromsø, Tromsø, Norway.

8. Faculty of Archaeology, Leiden University, Leiden, Netherlands.

9. Joint International Research Laboratory of Environment and Social Archaeology, Shandong University, Qingdao, China.

10. Department of Earth Science, Bjerknes Centre for Climate Research, University of Bergen, Bergen, Norway.

11. Centre for Early Sapiens Behaviour (SapienCE), University of Bergen, Bergen, Norway.

Abstract

Paleo-archives are essential for our understanding of species responses to climate warming, yet such archives are extremely rare in the Arctic. Here, we combine morphological analyses and bulk-bone metabarcoding to investigate a unique chronology of bone deposits sealed in the high-latitude Storsteinhola cave system (68°50′ N 16°22′ E) in Norway. This deposit dates to a period of climate warming from the end of the Late Glacial [~13 thousand calibrated years before the present (ka cal B.P.)] to the Holocene thermal maximum (~5.6 ka cal B.P.). Paleogenetic analyses allow us to exploit the 1000s of morphologically unidentifiable bone fragments resulting in a high-resolution sequence with 40 different taxa, including species not previously found here. Our record reveals borealization in both the marine and terrestrial environments above the Arctic Circle as a naturally recurring phenomenon in past periods of warming, providing fundamental insights into the ecosystem-wide responses that are ongoing today.

Publisher

American Association for the Advancement of Science (AAAS)

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