The Late Holocene deglaciation of James Ross Island, Antarctic Peninsula: OSL and 14C-dated multi-proxy sedimentary record from Monolith Lake-Reference-Cited by-同舟云学术

The Late Holocene deglaciation of James Ross Island, Antarctic Peninsula: OSL and 14C-dated multi-proxy sedimentary record from Monolith Lake

Published:2024-06 Issue: Volume:333 Page:108693
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Roman Matěj^ORCID,Píšková Anna,Sanderson David C.W.,Cresswell Alan J.,Bulínová Marie^ORCID,Pokorný Matěj^ORCID,Kavan Jan^ORCID,Jennings Stephen J.A.^ORCID,Lirio Juan M.^ORCID,Nedbalová Linda^ORCID,Sacherová Veronika^ORCID,Kopalová Kateřina^ORCID,Glasser Neil F.^ORCID,Nývlt Daniel^ORCID

Funder

Institute of Botany of the Czech Academy of Sciences

Univerzita Karlova v Praze

Ministerstvo Školství, Mládeže a Tělovýchovy

Grantová Agentura České Republiky

Publisher

Elsevier BV

Reference156 articles.

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3. Biogeochemical evidence for hydrologic changes during the Holocene in a lake sediment record from southeast Greenland;Balascio;Holocene,2013

4. Exposure-age record of Holocene ice sheet and ice shelf change in the northeast Antarctic Peninsula;Balco;Quat. Sci. Rev.,2013

5. Vegetation mapping of moss-dominated areas of northern part of James Ross Island (Antarctica) and a suggestion of protective measures;Barták;Czech Polar Rep,2015

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1. Accelerated retreat of northern James Ross Island ice streams (Antarctic Peninsula) in the Early-Middle Holocene induced by buoyancy response to postglacial sea level rise;Earth and Planetary Science Letters;2024-09