Coupling between biota and earth materials in the Critical Zone

被引:132
作者
Amundson, Ronald
Richter, Daniel D.
Humphreys, Geoff S.
Jobbagy, Esteban G.
Gaillardet, Jerome
机构
[1] Univ Calif Berkeley, Div Ecosyst Sci, Berkeley, CA 94720 USA
[2] Duke Univ, Nicholas Sch, Div Environm Sci & Policy, Durham, NC 27708 USA
[3] Macquarie Univ, Dept Phys Geog, N Ryde, NSW 2109, Australia
[4] Univ Nacl San Luis, IMASL, Grp Estudios Ambientales, San Luis, Argentina
[5] Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina
[6] Univ Paris 07, Lab Geochim Cosmochim, Inst Phys Globe, CNRS,UMR 7579, F-75252 Paris 05, France
关键词
chemical weathering; erosion; soils; biosphere;
D O I
10.2113/gselements.3.5.327
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The surface of our planet is the result of billions of years of feedback between biota and Earth materials. The chemical weathering of soils and the resulting stream and ocean chemistry bear the signature of the biological world. physical shaping of the Earth's surface in man re ions is a biologically mediated process. Given the pervasiveness of life, it is challenging to disentangle abiotic from biotic processes during field observations, yet it is of paramount importance to quantify these interactions and their feedbacks as the human impact on climate and ecosystems becomes more profound. Here we briefly review the fascinating connection between rocks and life and highlight its significance to science and society.
引用
收藏
页码:327 / 332
页数:6
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