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Euendolithic cyanobacteria/cyanophyta and their traces in Earth history

Identifieur interne : 00C753 ( Main/Exploration ); précédent : 00C752; suivant : 00C754

Euendolithic cyanobacteria/cyanophyta and their traces in Earth history

Auteurs : I. Glaub [Allemagne] ; S.-J. Balog [Allemagne] ; M. Bundschuh [Allemagne] ; M. Gektidis [Allemagne] ; K. Hofmann [Allemagne] ; G. Radtke [Allemagne] ; H. Schmidt [Allemagne] ; K. Vogel [Allemagne]

Source :

RBID : Pascal:00-0052168

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English descriptors

Abstract

The fossil microborings Fasciculus acinosus, Fasciculus dactylus, Eurygonum nodosum, and Scolecia filosa are taxa of traces, called ichnotaxa. Their morphology indicates that they are produced by once-living euendolithic cyanobacteria/cyanophyta from marine environments. Hyella spp., Solentia sp. (both Pleurocapsales), Mastigocoleus testarum (Stigonematales), and Plectonema terebrans (Nostocales) are their modern counterparts. The four ichnotaxa occur in Paleozoic (230 Ma to 570 Ma ago), Mesozoic (65 Ma to 230 Ma ago), and Cenozoic (65 Ma to Recent) strata. They differ in stratigraphic distribution within these eras. The bathymetric distribution patterns of Fasciculus acinosus, Fasciculus dactylus, and Scolecia filosa concur with those of their modern counterparts, whereas for Eurygonum nodosum differences are observed. The four ichnotaxa are of great importance to the reconstruction of paleo-depths.


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Le document en format XML

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<div type="abstract" xml:lang="en">The fossil microborings Fasciculus acinosus, Fasciculus dactylus, Eurygonum nodosum, and Scolecia filosa are taxa of traces, called ichnotaxa. Their morphology indicates that they are produced by once-living euendolithic cyanobacteria/cyanophyta from marine environments. Hyella spp., Solentia sp. (both Pleurocapsales), Mastigocoleus testarum (Stigonematales), and Plectonema terebrans (Nostocales) are their modern counterparts. The four ichnotaxa occur in Paleozoic (230 Ma to 570 Ma ago), Mesozoic (65 Ma to 230 Ma ago), and Cenozoic (65 Ma to Recent) strata. They differ in stratigraphic distribution within these eras. The bathymetric distribution patterns of Fasciculus acinosus, Fasciculus dactylus, and Scolecia filosa concur with those of their modern counterparts, whereas for Eurygonum nodosum differences are observed. The four ichnotaxa are of great importance to the reconstruction of paleo-depths.</div>
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