Triploblastic animals more than 1 billion years ago:: Trace fossil evidence from India

被引:173
作者
Seilacher, A [1 ]
Bose, PK
Pflüger, F
机构
[1] Univ Tubingen, Inst Geol Palaontol, D-72076 Tubingen, Germany
[2] Yale Univ, Dept Geol & Geophys, New Haven, CT 06520 USA
[3] Jadavpur Univ, Dept Geol Sci, Calcutta 700032, W Bengal, India
关键词
D O I
10.1126/science.282.5386.80
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
Some intriguing bedding plane features that were observed in the Meso-proterozoic Chorhat Sandstone are biological and can be interpreted as the burrows of wormlike undermat miners (that is, infaunal animals that excavated tunnels underneath microbial mats), These burrows suggest that triploblastic animals existed more than a billion years ago. They also suggest that the diversification of animal designs proceeded very slowly before the appearance of organisms with hard skeletons, which was probably the key event in the Cambrian evolutionary explosion, and before the ecological changes that accompanied that event.
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页码:80 / 83
页数:6
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