The responses of the terrestrial carbon cycle to global change across the Paleocene/Eocene boundary

被引:1
作者
Beerling, DJ [1 ]
机构
[1] Univ Sheffield, Dept Anim & Plant Sci, Sheffield S10 2TN, S Yorkshire, England
关键词
D O I
10.1080/11035890001221023
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
[No abstract available]
引用
收藏
页码:23 / 23
页数:1
相关论文
共 4 条
[1]  
BEERLING DJ, IN PRESS PALAEOGEOGR
[2]  
Dickens GR, 1997, GEOLOGY, V25, P259, DOI 10.1130/0091-7613(1997)025<0259:ABOGIT>2.3.CO
[3]  
2
[4]   DISSOCIATION OF OCEANIC METHANE HYDRATE AS A CAUSE OF THE CARBON-ISOTOPE EXCURSION AT THE END OF THE PALEOCENE [J].
DICKENS, GR ;
ONEIL, JR ;
REA, DK ;
OWEN, RM .
PALEOCEANOGRAPHY, 1995, 10 (06) :965-971