TRACE FOSSILS FROM PRECAMBRIAN AND BASAL CAMBRIAN

被引：184

作者：

GLAESSNER, MF

机构：

[1] Department of Geology, University of Adelaide, Adelaide

来源：

LETHAIA | 1969年 / 2卷 / 04期

关键词：

D O I：

10.1111/j.1502-3931.1969.tb01258.x

中图分类号：

Q91 [古生物学];

学科分类号：

0709 ; 070903 ;

摘要：

Certain worm‐like configurations on rocks are recognized as shrinkage‐crack infillings. Some genuine Precambrian trace fossils are briefly described. The early Cambrian contains a richer assemblage, including some distinctive and widespread form genera. The study of early trace fossils leads to conclusions not only on facies, but also on the evolution of behaviour and functional morphology in soft‐bodied organisms. Copyright © 1969, Wiley Blackwell. All rights reserved

引用

页码：369 / +

页数：1

共 51 条

[1]

ALF RM, 1959, PLATEAU, V31, P60

[2]

ALTAVOGT G, 1968, N J GEOL PALAONT ABH, V132, P1

[3]

BANDEL K, 1967, U KANSAS PALEONT CON, V18

[4] GEOLOGY - SOME MARKINGS ASSOCIATED WITH RIPPLE-MARKS FROM PROTEROZOIC OF NORTH AMERICA [J].

BARNES, WC ;

SMITH, AG .

NATURE, 1964, 201 (492) :1018-&

[5]

Cloud P. E. Jr., 1968, P1

[6] PHANEROZOIC-CRYPTOZOIC AND RELATED TRANSITIONS - NEW EVIDENCE [J].

CLOUD, PE ;

NELSON, CA .

SCIENCE, 1966, 154 (3750) :766-&

[7]

DALGARNO C. R., 1964, T ROYAL SOC S AUSTR, V88, P129

[8]

Dawson J.W., 1890, Q J GEOLOGICAL SOC S, V46, P595, DOI DOI 10.1144/GSL.JGS.1890.046.01-04.39

[9]

ENDO RIUJI, 1933, JAPANESE JOUR GEOL AND GEOGR, V11, P43

[10]

Farrow G. E., 1966, Palaeogeography Palaeoclimatology Palaeoecology, V2, P103, DOI 10.1016/0031-0182(66)90011-3

← 1 2 3 4 5 6 →