Relative Paleoenvironmental Adjustments Following Deglaciation of the Byers Peninsula (Livingston Island, Antarctica)-Reference-Cited by-同舟云学术

Relative Paleoenvironmental Adjustments Following Deglaciation of the Byers Peninsula (Livingston Island, Antarctica)

Published:2016-05 Issue:2 Volume:48 Page:345-359
ISSN:1523-0430
Container-title:Arctic, Antarctic, and Alpine Research
language:en
Short-container-title:Arctic, Antarctic, and Alpine Research

Author:

Ruiz-Fernández Jesús¹,Oliva Marc²

Affiliation:

1. Department of Geography, University of Oviedo, Teniente Alfonso Martínez s/n, 33011, Oviedo, Spain

2. Centre for Geographical Studies—Institute of Geography and Spatial Planning, University of Lisbon, Alameda da Universidade, 1600-214, Lisbon, Portugal

Publisher

Informa UK Limited

Subject

Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Link

https://www.tandfonline.com/doi/pdf/10.1657/AAAR0015-014

Reference63 articles.

1. Exposure-age record of Holocene ice sheet and ice shelf change in the northeast Antarctic Peninsula

2. Paraglacial geomorphology

3. A general model of paraglacial landscape response

4. Regional weather survey on Byers Peninsula, Livingston Island, South Shetland Islands, Antarctica

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1. Signals of soil formation during pre-glacial maximum on the byers peninsula (maritime antarctica);CATENA;2024-10

2. Interannual variability of ground surface thermal regimes in Livingston and Deception islands, Antarctica (2007–2021);Land Degradation & Development;2023-10-24

3. Soil organic matter accumulation before, during, and after the last glacial maximum in Byers Peninsula, Maritime Antarctica;Geoderma;2022-12

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