Do Cryoconite Holes have the Potential to be Significant Sources of C, N, and P to Downstream Depauperate Ecosystems of Taylor Valley, Antarctica?-Reference-Cited by-同舟云学术

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Do Cryoconite Holes have the Potential to be Significant Sources of C, N, and P to Downstream Depauperate Ecosystems of Taylor Valley, Antarctica?

Published:2013-11 Issue:4 Volume:45 Page:440-454
ISSN:1523-0430
Container-title:Arctic, Antarctic, and Alpine Research
language:en
Short-container-title:Arctic, Antarctic, and Alpine Research

Author:

Bagshaw Elizabeth A.¹,Tranter Martyn¹,Fountain Andrew G.²,Welch Kathleen³,Basagic Hassan J.²,Lyons W. Berry³

Affiliation:

1. Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, University Road, Clifton, Bristol BS8 1SS, U.K.

2. Departments of Geography and Geology, Portland State University, P.O. Box 751, Portland, Oregon 97207-0751, U.S.A.

3. Byrd Polar Research Center, Ohio State University, 1090 Carmack Road, Columbus, Ohio 43210–1002, U.S.A.

Publisher

Informa UK Limited

Subject

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

Link

https://www.tandfonline.com/doi/pdf/10.1657/1938-4246-45.4.440

Reference75 articles.

1. Biogeochemical evolution of cryoconite holes on Canada Glacier, Taylor Valley, Antarctica

2. Implications of meltwater pulse events for soil biology and biogeochemical cycling in a polar desert

3. VARIATION IN BIOGEOCHEMISTRY AND SOIL BIODIVERSITY ACROSS SPATIAL SCALES IN A POLAR DESERT ECOSYSTEM

4. Soil carbon turnover in the McMurdo Dry Valleys, Antarctica

5. Biogeochemical stoichiometry of Antarctic Dry Valley ecosystems

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