ISOTOPIC BIOGEOCHEMISTRY OF CARBON IN RECENT AND FOSSIL MAMMAL BONES AND TEETH FROM COLD TEMPERATURE AREAS

被引：0
|
作者：
BOCHERENS, H
MARIOTTI, A
机构：
来源：
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II | 1992年 / 315卷 / 09期
关键词：
PALEONTOLOGY; GEOCHEMISTRY;
D O I：
暂无
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
The difference between C-13 isotopic abundances in bone organic matter (collagen) and the mineral phase (carbonate hydroxylapatite) is used for the determination of the trophic level of the animal, especially on fossil samples. This difference is greater for herbivore mammals from cold and temperate areas than for South African herbivore mammals studied previously (8.4 +/- 1.4 parts per thousand versus 6.8 +/- 1.4 parts per thousand respectively). This larger value should be used in the interpretation of isotopic abundances of C-13 in fossil mammals from temperate and arctic areas.
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页码：1147 / 1153
页数：7
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