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Updated: Jul 20, 2026

Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential
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Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential

Published on: April 20, 2012

Desglaciación del Holoceno de la Tierra Marie Byrd, en el oeste de la Antártida

John O Stone1, Gregory A Balco, David E Sugden

  • 1Quaternary Research Center and Department of Earth and Space Sciences, Box 351360, University of Washington, Seattle, WA 98195-1360, USA. stone@geology.washington.edu

Science (New York, N.Y.)
|January 4, 2003
PubMed
Resumen

La capa de hielo de la Antártida Occidental se ha estado adelgazando continuamente durante 10.000 años, retrasando la desglaciación del hemisferio norte. Esta disminución a largo plazo aún puede estar en curso, lo que contribuye al aumento del nivel del mar.

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