Individual to community-level faunal responses to environmental change from a marine fossil record of Early Miocene global warming.

Modern climate change has a strong potential to shift earth systems and biological communities into novel states that have no present-day analog, leaving ecologists with no observational basis to predict the likely biotic effects. Fossil records contain long time-series of past environmental changes...

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Autor principal: Christina L Belanger
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Publicado: Public Library of Science (PLoS) 2012
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Acceso en línea:https://doaj.org/article/9e1f366fd98d43978bbe60b4b99fa863
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spelling oai:doaj.org-article:9e1f366fd98d43978bbe60b4b99fa8632021-11-18T07:20:18ZIndividual to community-level faunal responses to environmental change from a marine fossil record of Early Miocene global warming.1932-620310.1371/journal.pone.0036290https://doaj.org/article/9e1f366fd98d43978bbe60b4b99fa8632012-01-01T00:00:00Zhttps://www.ncbi.nlm.nih.gov/pmc/articles/pmid/22558424/?tool=EBIhttps://doaj.org/toc/1932-6203Modern climate change has a strong potential to shift earth systems and biological communities into novel states that have no present-day analog, leaving ecologists with no observational basis to predict the likely biotic effects. Fossil records contain long time-series of past environmental changes outside the range of modern observation, which are vital for predicting future ecological responses, and are capable of (a) providing detailed information on rates of ecological change, (b) illuminating the environmental drivers of those changes, and (c) recording the effects of environmental change on individual physiological rates. Outcrops of Early Miocene Newport Member of the Astoria Formation (Oregon) provide one such time series. This record of benthic foraminiferal and molluscan community change from continental shelf depths spans a past interval environmental change (≈ 20.3-16.7 mya) during which the region warmed 2.1-4.5°C, surface productivity and benthic organic carbon flux increased, and benthic oxygenation decreased, perhaps driven by intensified upwelling as on the modern Oregon coast. The Newport Member record shows that (a) ecological responses to natural environmental change can be abrupt, (b) productivity can be the primary driver of faunal change during global warming, (c) molluscs had a threshold response to productivity change while foraminifera changed gradually, and (d) changes in bivalve body size and growth rates parallel changes in taxonomic composition at the community level, indicating that, either directly or indirectly through some other biological parameter, the physiological tolerances of species do influence community change. Ecological studies in modern and fossil records that consider multiple ecological levels, environmental parameters, and taxonomic groups can provide critical information for predicting future ecological change and evaluating species vulnerability.Christina L BelangerPublic Library of Science (PLoS)articleMedicineRScienceQENPLoS ONE, Vol 7, Iss 4, p e36290 (2012)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Christina L Belanger
Individual to community-level faunal responses to environmental change from a marine fossil record of Early Miocene global warming.
description Modern climate change has a strong potential to shift earth systems and biological communities into novel states that have no present-day analog, leaving ecologists with no observational basis to predict the likely biotic effects. Fossil records contain long time-series of past environmental changes outside the range of modern observation, which are vital for predicting future ecological responses, and are capable of (a) providing detailed information on rates of ecological change, (b) illuminating the environmental drivers of those changes, and (c) recording the effects of environmental change on individual physiological rates. Outcrops of Early Miocene Newport Member of the Astoria Formation (Oregon) provide one such time series. This record of benthic foraminiferal and molluscan community change from continental shelf depths spans a past interval environmental change (≈ 20.3-16.7 mya) during which the region warmed 2.1-4.5°C, surface productivity and benthic organic carbon flux increased, and benthic oxygenation decreased, perhaps driven by intensified upwelling as on the modern Oregon coast. The Newport Member record shows that (a) ecological responses to natural environmental change can be abrupt, (b) productivity can be the primary driver of faunal change during global warming, (c) molluscs had a threshold response to productivity change while foraminifera changed gradually, and (d) changes in bivalve body size and growth rates parallel changes in taxonomic composition at the community level, indicating that, either directly or indirectly through some other biological parameter, the physiological tolerances of species do influence community change. Ecological studies in modern and fossil records that consider multiple ecological levels, environmental parameters, and taxonomic groups can provide critical information for predicting future ecological change and evaluating species vulnerability.
format article
author Christina L Belanger
author_facet Christina L Belanger
author_sort Christina L Belanger
title Individual to community-level faunal responses to environmental change from a marine fossil record of Early Miocene global warming.
title_short Individual to community-level faunal responses to environmental change from a marine fossil record of Early Miocene global warming.
title_full Individual to community-level faunal responses to environmental change from a marine fossil record of Early Miocene global warming.
title_fullStr Individual to community-level faunal responses to environmental change from a marine fossil record of Early Miocene global warming.
title_full_unstemmed Individual to community-level faunal responses to environmental change from a marine fossil record of Early Miocene global warming.
title_sort individual to community-level faunal responses to environmental change from a marine fossil record of early miocene global warming.
publisher Public Library of Science (PLoS)
publishDate 2012
url https://doaj.org/article/9e1f366fd98d43978bbe60b4b99fa863
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