Shell laminae and shell orientation in the upper Silurian, Overton Formation, U.K-Reference-Cited by-同舟云学术

Shell laminae and shell orientation in the upper Silurian, Overton Formation, U.K

Published:1980-01 Issue: Volume:32 Page:119-133
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Antia David D.J.

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference41 articles.

1. A quantitative study of the origin of Dreissena polymorpha shell accumulations in Szczecin Bay, Baltic Sea;Alexandrowicz;Bull. Acad. Pol. Sci.,1978

2. Statiscical inference about Markov Chains;Anderson;Ann. Math. Statist.,1957

3. Bone-beds: a review of their classification, occurrence, genesis, diagenesis, geochemistry, palaeoecology, weathering, and microbiotas;Antia;Mercian Geol.,1979

4. Authigenic gypsum in marine sediments — a comment;Antia;Mar. Geol.,1979

5. Comments on the environments and faunas across the Ludlovian—Downtonian boundary (Upper Silurian) at Siefton, Salop;Antia;Geol. J.,1979

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2. The Evolution of Infaunal Communities and Sedimentary Fabrics;Topics in Geobiology;1983

3. Sediment-Mediated Biological Disturbance and the Evolution of Marine Benthos;Topics in Geobiology;1983

4. Ludlow stratigraphy at Ludlow, Shropshire;Geological Magazine;1982-11