Trace fossils indicating bottom aeration changes: Folusz Limestone, Oligocene, Outer Carpathians, Poland

Trace fossils indicating bottom aeration changes: Folusz Limestone, Oligocene, Outer Carpathians, Poland

Bioturbation sequences in the pelagic Folusz limestone indicate deposition under decreasing bottom aeration, possibly in association with the development of microbial mats. U-shaped burrows Diplocraterion and Arenicolites exclusively were produced in the laminated limestone, and they represent the o...

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Veröffentlicht in:Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 1996-04, Vol.121 (1), p.79-87
Hauptverfasser: Leszczynski, Stanislaw, Uchman, Alfred, Bromley, Richard G.
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Sprache:eng
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Marine
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container_title Palaeogeography, palaeoclimatology, palaeoecology
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creator Leszczynski, Stanislaw
Uchman, Alfred
Bromley, Richard G.
description Bioturbation sequences in the pelagic Folusz limestone indicate deposition under decreasing bottom aeration, possibly in association with the development of microbial mats. U-shaped burrows Diplocraterion and Arenicolites exclusively were produced in the laminated limestone, and they represent the only colonizers (sessile suspension feeders) of the oxygen-deficient sediment.
doi_str_mv 10.1016/0031-0182(95)00052-6
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language eng
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source Elsevier ScienceDirect Journals
subjects Marine
title Trace fossils indicating bottom aeration changes: Folusz Limestone, Oligocene, Outer Carpathians, Poland
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