Geochemical signature of incremental growth; rugose corals from the Middle Devonian Traverse Group, Michigan

Incremental growth has long been known in living and fossil scleractinian corals, and also has been recognized in Paleozoic rugose and tabulate corals. The usefulness of growth studies and geochemistry has been demonstrated in the study of environmental aspects and population structure of modern and...

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Veröffentlicht in:	Palaios 1996-02, Vol.11 (1), p.64-70
1. Verfasser:	Sorauf, James E
Format:	Artikel
Sprache:	eng
Schlagworte:	alkaline earth metals Anthozoa biogenic processes Calcite Carbonates Charlevoix County Michigan Cnidaria Coelenterata Corals Devonian electron probe data Electrons Emmet County Michigan epibiotism Fibrous minerals Fossils Geochemistry Givetian Gravel Point Formation growth indicators Invertebrata invertebrate Magnesium metals Michigan Michigan Lower Peninsula microstructure Middle Devonian morphology outcrops Paleontology Paleozoic Research Letters rock, sediment, soil Rugosa Sea water SEM data septa Skeleton spatial distribution Tabulophyllum traversensis trace elements Traverse Group United States Zoantharia
Online-Zugang:	Volltext
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