Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity

Silurian turreted gastropods from the Upper Leintwardine Formation, Ludlow Series, collected in Delbury Quarry, Shropshire, UK, are all encrusted by the trepostome bryozoan Homotrypa cochlea sp. nov. Bryozoans were not found to encrust any other component of the shelly fauna and thus seemed pref...

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Main Authors: CAROLINE J. BUTTLER, LESLEY CHERNS, LUCY M.E. MCCOBB
Format: Article
Language:English
Published: Institute of Paleobiology PAS 2022-09-01
Series:Acta Palaeontologica Polonica
Subjects:
Online Access:https://www.app.pan.pl/archive/published/app67/app009642021.pdf
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author CAROLINE J. BUTTLER
LESLEY CHERNS
LUCY M.E. MCCOBB
author_facet CAROLINE J. BUTTLER
LESLEY CHERNS
LUCY M.E. MCCOBB
author_sort CAROLINE J. BUTTLER
collection DOAJ
description Silurian turreted gastropods from the Upper Leintwardine Formation, Ludlow Series, collected in Delbury Quarry, Shropshire, UK, are all encrusted by the trepostome bryozoan Homotrypa cochlea sp. nov. Bryozoans were not found to encrust any other component of the shelly fauna and thus seemed preferentially to choose the gastropod shells. The relationship between these two organisms was examined to consider whether the bryozoans were using the dead, empty mollusc shells as a substrate, if they were living symbiotically with live gastropods, or if the shells were inhabited by a non-gastropod host. There is evidence that the bryozoans encrusted the shells of living gastropods but continued growing after the death of the mollusc, potentially with the shell then occupied by a conchicole. Bryozoans encased the gastropod shells and, after death of the mollusc, the internal cavity became a “closed” microenvironment where the shell form and sometimes the recrystallised shell became preserved. The aragonitic shells of these gastropods were prone to dissolution early in diagenesis, and no gastropods are found without encrusting bryozoans. Bryoimmuration resulted in a local taphonomic window for the molluscs, which are notably sparse in most early Palaeozoic shelly faunas—the so-called “missing molluscs” phenomenon.
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spelling doaj.art-84bd1f4c40a742cc89d0c8229b22f2572022-12-22T04:03:26ZengInstitute of Paleobiology PASActa Palaeontologica Polonica0567-79201732-24212022-09-0167356957710.4202/app.00964.2021Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversityCAROLINE J. BUTTLER0LESLEY CHERNS1LUCY M.E. MCCOBB2Department of Natural Sciences, Amgueddfa Cymru National Museum Wales, Cathays Park, Cardiff CF10 3NP, Wales, UK.School of Earth and Environmental Sciences, Cardiff University, Cardiff CF10 3AT, Wales, UK.Department of Natural Sciences, Amgueddfa Cymru National Museum Wales, Cathays Park, Cardiff CF10 3NP, Wales, UK.Silurian turreted gastropods from the Upper Leintwardine Formation, Ludlow Series, collected in Delbury Quarry, Shropshire, UK, are all encrusted by the trepostome bryozoan Homotrypa cochlea sp. nov. Bryozoans were not found to encrust any other component of the shelly fauna and thus seemed preferentially to choose the gastropod shells. The relationship between these two organisms was examined to consider whether the bryozoans were using the dead, empty mollusc shells as a substrate, if they were living symbiotically with live gastropods, or if the shells were inhabited by a non-gastropod host. There is evidence that the bryozoans encrusted the shells of living gastropods but continued growing after the death of the mollusc, potentially with the shell then occupied by a conchicole. Bryozoans encased the gastropod shells and, after death of the mollusc, the internal cavity became a “closed” microenvironment where the shell form and sometimes the recrystallised shell became preserved. The aragonitic shells of these gastropods were prone to dissolution early in diagenesis, and no gastropods are found without encrusting bryozoans. Bryoimmuration resulted in a local taphonomic window for the molluscs, which are notably sparse in most early Palaeozoic shelly faunas—the so-called “missing molluscs” phenomenon.https://www.app.pan.pl/archive/published/app67/app009642021.pdfgastropodabryozoasymbiosisovergrowtharagonitetaphonomysilurianshropshireuk
spellingShingle CAROLINE J. BUTTLER
LESLEY CHERNS
LUCY M.E. MCCOBB
Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity
Acta Palaeontologica Polonica
gastropoda
bryozoa
symbiosis
overgrowth
aragonite
taphonomy
silurian
shropshire
uk
title Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity
title_full Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity
title_fullStr Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity
title_full_unstemmed Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity
title_short Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity
title_sort trepostome bryozoans encrusting silurian gastropods a taphonomic window and its implications for biodiversity
topic gastropoda
bryozoa
symbiosis
overgrowth
aragonite
taphonomy
silurian
shropshire
uk
url https://www.app.pan.pl/archive/published/app67/app009642021.pdf
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AT lesleycherns trepostomebryozoansencrustingsiluriangastropodsataphonomicwindowanditsimplicationsforbiodiversity
AT lucymemccobb trepostomebryozoansencrustingsiluriangastropodsataphonomicwindowanditsimplicationsforbiodiversity