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Late Pleistocene shrub expansion preceded megafauna turnover and extinctions in eastern Beringia

Late Pleistocene shrub expansion preceded megafauna turnover and extinctions in eastern Beringia
Late Pleistocene shrub expansion preceded megafauna turnover and extinctions in eastern Beringia

The collapse of the steppe-tundra biome (mammoth steppe) at the end of the Pleistocene is used as an important example of topdown ecosystem cascades, where human hunting of keystone species led to profound changes in vegetation across high latitudes in the Northern Hemisphere. Alternatively, it is argued that this biome transformation occurred through a bottom-up process, where climate-driven expansion of shrub tundra (Betula, Salix spp.) replaced the steppe-tundra vegetation that grazing megafauna taxa relied on. In eastern Beringia, these differing hypotheses remain largely untested, in part because the precise timing and spatial pattern of Late Pleistocene shrub expansion remains poorly resolved. This uncertainty is caused by chronological ambiguity in many lake sediment records, which typically rely on radiocarbon (14C) dates from bulk sediment or aquatic macrofossils-materials that are known to overestimate the age of sediment layers. Here, we reexamine Late Pleistocene pollen records for which 14C dating of terrestrial macrofossils is available and augment these data with 14C dates from arctic ground-squirrel middens and plant macrofossils. Comparing these paleovegetation data with a database of published 14C dates from megafauna remains, we find the postglacial expansion of shrub tundra preceded the regional extinctions of horse (Equus spp.) and mammoth (Mammuthus primigenius) and began during a period when the frequency of 14C dates indicates large grazers were abundant. These results are not consistent with a model of top-down ecosystem cascades and support the hypothesis that climate-driven habitat loss preceded and contributed to turnover in mammal communities.

megafauna, eastern Beringia, keystone species, palaeoecology, steppetundra
0027-8424
Monteath, Alistair J.
d9499e7f-b5d9-48ad-87d8-3c2a74e40fa9
Gaglioti, Benjamin V.
03e8c0a3-08b3-44b3-b463-b9d13f186731
Edwards, Mary E.
4b6a3389-f3a4-4933-b8fd-acdfef72200e
Froese, Duane
f680a186-8426-4505-8c68-09fb85b3e5fe
Monteath, Alistair J.
d9499e7f-b5d9-48ad-87d8-3c2a74e40fa9
Gaglioti, Benjamin V.
03e8c0a3-08b3-44b3-b463-b9d13f186731
Edwards, Mary E.
4b6a3389-f3a4-4933-b8fd-acdfef72200e
Froese, Duane
f680a186-8426-4505-8c68-09fb85b3e5fe

Monteath, Alistair J., Gaglioti, Benjamin V., Edwards, Mary E. and Froese, Duane (2021) Late Pleistocene shrub expansion preceded megafauna turnover and extinctions in eastern Beringia. Proceedings of the National Academy of Sciences of the United States of America, 118 (52), [e2107977118]. (doi:10.1073/pnas.2107977118).

Record type: Article

Abstract

The collapse of the steppe-tundra biome (mammoth steppe) at the end of the Pleistocene is used as an important example of topdown ecosystem cascades, where human hunting of keystone species led to profound changes in vegetation across high latitudes in the Northern Hemisphere. Alternatively, it is argued that this biome transformation occurred through a bottom-up process, where climate-driven expansion of shrub tundra (Betula, Salix spp.) replaced the steppe-tundra vegetation that grazing megafauna taxa relied on. In eastern Beringia, these differing hypotheses remain largely untested, in part because the precise timing and spatial pattern of Late Pleistocene shrub expansion remains poorly resolved. This uncertainty is caused by chronological ambiguity in many lake sediment records, which typically rely on radiocarbon (14C) dates from bulk sediment or aquatic macrofossils-materials that are known to overestimate the age of sediment layers. Here, we reexamine Late Pleistocene pollen records for which 14C dating of terrestrial macrofossils is available and augment these data with 14C dates from arctic ground-squirrel middens and plant macrofossils. Comparing these paleovegetation data with a database of published 14C dates from megafauna remains, we find the postglacial expansion of shrub tundra preceded the regional extinctions of horse (Equus spp.) and mammoth (Mammuthus primigenius) and began during a period when the frequency of 14C dates indicates large grazers were abundant. These results are not consistent with a model of top-down ecosystem cascades and support the hypothesis that climate-driven habitat loss preceded and contributed to turnover in mammal communities.

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More information

e-pub ahead of print date: 20 December 2021
Published date: 28 December 2021
Additional Information: Funding Information: Data Availability. All study data are included in the article and/or supporting information. Previously published data were used for this work. (The supporting information for this manuscript includes a database of published radiocarbon dates. The original studies for these dates are cited, and there are no copyright issues.) ACKNOWLEDGMENTS. We are grateful to Nancy Bigelow, Yue Wang, Joshua Kurek, Darrell Kaufman, Scott Anderson, Petra Boltshauser-Kaltenrieder, Willy Tinner, César Morales, and Jesse Vermaire, who provided access to palaeoecological datasets from study sites in eastern Beringia. The project was supported by a Natural Sciences and Engineering Research Council Canada grant as part of the Future ArcTic Ecosystems (FATE) project. Ben Gaglioti was supported by NSF grant OPP-1850578. The comments from two anonymous reviewers helped to improve the clarity and focus of this manuscript. Publisher Copyright: © 2021 National Academy of Sciences. All rights reserved. Copyright: Copyright 2022 Elsevier B.V., All rights reserved.
Keywords: megafauna, eastern Beringia, keystone species, palaeoecology, steppetundra

Identifiers

Local EPrints ID: 454448
URI: http://eprints.soton.ac.uk/id/eprint/454448
ISSN: 0027-8424
PURE UUID: 87a7684d-ba1e-47a0-9dc2-49695a4e80cb
ORCID for Mary E. Edwards: ORCID iD orcid.org/0000-0002-3490-6682

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Date deposited: 09 Feb 2022 17:44
Last modified: 18 Mar 2024 02:55

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Contributors

Author: Alistair J. Monteath
Author: Benjamin V. Gaglioti
Author: Mary E. Edwards ORCID iD
Author: Duane Froese

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