Global peatland dynamics since the Last Glacial Maximum

Author:

Yu Zicheng1,Loisel Julie1,Brosseau Daniel P.1,Beilman David W.2,Hunt Stephanie J.1

Affiliation:

1. Department of Earth and Environmental Sciences; Lehigh University; Bethlehem; Pennsylvania; USA

2. Department of Geography; University of Hawai'i at Mānoa; Honolulu; Hawaii; USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference28 articles.

1. Interhemispheric Atlantic seesaw response during the last deglaciation;Barker;Science,2009

2. On the origin and timing of rapid changes in atmospheric methane during the last glacial period;Brook;Global Biogeochem. Cycles,2000

3. Changes in the atmospheric CH4 gradient between Greenland and Antarctica during the Holocene;Chappellaz;J. Geophys. Res.,1997

4. Carbon accumulation in peatland;Clymo;Oikos,1998

5. Stable isotope constraints on Holocene carbon cycle changes from an Antarctic ice core;Elsig;Nature,2009

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