Large trilobites in a stress-free Early Ordovician environment
Understanding variations in body size is essential for deciphering the response of an organism to its surrounding environmental conditions and its ecological adaptations. In modern environments, large marine animals are mostly found in cold waters. However, numerous parameters can influence body-siz...
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Veröffentlicht in: | Geological magazine 2021-02, Vol.158 (2), p.261-270 |
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creator | Saleh, Farid Vidal, Muriel Laibl, Lukáš Sansjofre, Pierre Gueriau, Pierre Pérez-Peris, Francesc Lustri, Lorenzo Lucas, Victoire Lefebvre, Bertrand Pittet, Bernard El Hariri, Khadija Daley, Allison C. |
description | Understanding variations in body size is essential for deciphering the response of an organism to its surrounding environmental conditions and its ecological adaptations. In modern environments, large marine animals are mostly found in cold waters. However, numerous parameters can influence body-size variations other than temperatures, such as oxygenation, nutrient availability, predation or physical disturbances by storms. Here, we investigate trilobite size variations in the Lower Ordovician Fezouata Shale deposited in a cold-water environment. Trilobite assemblages dominated by small- to normal-sized specimens that are a few centimetres in length are found in proximal and intermediate settings, while those comprising larger taxa more than 20 cm in length are found in the most distal environment of the Fezouata Shale. Drill core material from distal settings shows that sedimentary rocks hosting large trilobites preserved in situ are extensively bioturbated with a high diversity of trace fossils, indicating that oxygen and nutrients were available in this environment. In intermediate and shallow settings, bioturbation is less extensive and shallower in depth. The rarity of storm events (minimal physical disturbance) and the lack of predators in deep environments in comparison to shallower settings would also have helped trilobites attain larger body sizes. This highly resolved spatial study investigating the effects of numerous biotic and abiotic parameters on body size has wider implications for the understanding of size fluctuations over geological time. |
doi_str_mv | 10.1017/S0016756820000448 |
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In modern environments, large marine animals are mostly found in cold waters. However, numerous parameters can influence body-size variations other than temperatures, such as oxygenation, nutrient availability, predation or physical disturbances by storms. Here, we investigate trilobite size variations in the Lower Ordovician Fezouata Shale deposited in a cold-water environment. Trilobite assemblages dominated by small- to normal-sized specimens that are a few centimetres in length are found in proximal and intermediate settings, while those comprising larger taxa more than 20 cm in length are found in the most distal environment of the Fezouata Shale. Drill core material from distal settings shows that sedimentary rocks hosting large trilobites preserved in situ are extensively bioturbated with a high diversity of trace fossils, indicating that oxygen and nutrients were available in this environment. In intermediate and shallow settings, bioturbation is less extensive and shallower in depth. The rarity of storm events (minimal physical disturbance) and the lack of predators in deep environments in comparison to shallower settings would also have helped trilobites attain larger body sizes. This highly resolved spatial study investigating the effects of numerous biotic and abiotic parameters on body size has wider implications for the understanding of size fluctuations over geological time.</description><identifier>ISSN: 0016-7568</identifier><identifier>EISSN: 1469-5081</identifier><identifier>DOI: 10.1017/S0016756820000448</identifier><language>eng</language><publisher>Cambridge, UK: Cambridge University Press</publisher><subject>Abiotic factors ; Adaptation ; Africa ; Arthropoda ; biostratigraphy ; Bioturbation ; Body size ; clastic rocks ; Coring ; depositional environment ; Earth Sciences ; Ecological adaptation ; Environmental conditions ; Fezouata Shale ; Fossil animals ; Fossils ; Geological time ; Geology ; Interspecific relationships ; invertebrate ; Invertebrates ; Length ; Lower Ordovician ; Marine animals ; Marine invertebrates ; Marine organisms ; Mineral nutrients ; Morocco ; North Africa ; Nutrient availability ; Nutrients ; Ordovician ; Original Article ; Oxygenation ; paleoenvironment ; Paleontology ; Paleozoic ; Parameters ; Platypeltoides ; Predation ; Predators ; Sciences of the Universe ; Sedimentary rocks ; Shale ; Shales ; Storms ; Stratigraphy ; Trace fossils ; Trilobita ; Trilobitomorpha ; Variation ; Water temperature</subject><ispartof>Geological magazine, 2021-02, Vol.158 (2), p.261-270</ispartof><rights>The Author(s), 2020. Published by Cambridge University Press</rights><rights>GeoRef, Copyright 2021, American Geosciences Institute. Reference includes data from GeoScienceWorld @Alexandria, VA @USA @United States. Abstract, Copyright, Cambridge University Press</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a501t-1207811d8dad5c54a25812e92bfa5202b0e490b847f78e185e83b1c2e52666423</citedby><cites>FETCH-LOGICAL-a501t-1207811d8dad5c54a25812e92bfa5202b0e490b847f78e185e83b1c2e52666423</cites><orcidid>0000-0002-7529-3456 ; 0000-0002-9165-985X ; 0000-0002-4526-9308 ; 0000-0002-3803-9176 ; 0000-0001-9049-3811 ; 0000-0001-9617-1610</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0016756820000448/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>164,230,314,776,780,881,27901,27902,55603</link.rule.ids><backlink>$$Uhttps://hal.science/hal-03005087$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Saleh, Farid</creatorcontrib><creatorcontrib>Vidal, Muriel</creatorcontrib><creatorcontrib>Laibl, Lukáš</creatorcontrib><creatorcontrib>Sansjofre, Pierre</creatorcontrib><creatorcontrib>Gueriau, Pierre</creatorcontrib><creatorcontrib>Pérez-Peris, Francesc</creatorcontrib><creatorcontrib>Lustri, Lorenzo</creatorcontrib><creatorcontrib>Lucas, Victoire</creatorcontrib><creatorcontrib>Lefebvre, Bertrand</creatorcontrib><creatorcontrib>Pittet, Bernard</creatorcontrib><creatorcontrib>El Hariri, Khadija</creatorcontrib><creatorcontrib>Daley, Allison C.</creatorcontrib><title>Large trilobites in a stress-free Early Ordovician environment</title><title>Geological magazine</title><addtitle>Geol. Mag</addtitle><description>Understanding variations in body size is essential for deciphering the response of an organism to its surrounding environmental conditions and its ecological adaptations. In modern environments, large marine animals are mostly found in cold waters. However, numerous parameters can influence body-size variations other than temperatures, such as oxygenation, nutrient availability, predation or physical disturbances by storms. Here, we investigate trilobite size variations in the Lower Ordovician Fezouata Shale deposited in a cold-water environment. Trilobite assemblages dominated by small- to normal-sized specimens that are a few centimetres in length are found in proximal and intermediate settings, while those comprising larger taxa more than 20 cm in length are found in the most distal environment of the Fezouata Shale. Drill core material from distal settings shows that sedimentary rocks hosting large trilobites preserved in situ are extensively bioturbated with a high diversity of trace fossils, indicating that oxygen and nutrients were available in this environment. In intermediate and shallow settings, bioturbation is less extensive and shallower in depth. The rarity of storm events (minimal physical disturbance) and the lack of predators in deep environments in comparison to shallower settings would also have helped trilobites attain larger body sizes. This highly resolved spatial study investigating the effects of numerous biotic and abiotic parameters on body size has wider implications for the understanding of size fluctuations over geological time.</description><subject>Abiotic factors</subject><subject>Adaptation</subject><subject>Africa</subject><subject>Arthropoda</subject><subject>biostratigraphy</subject><subject>Bioturbation</subject><subject>Body size</subject><subject>clastic rocks</subject><subject>Coring</subject><subject>depositional environment</subject><subject>Earth Sciences</subject><subject>Ecological adaptation</subject><subject>Environmental conditions</subject><subject>Fezouata Shale</subject><subject>Fossil animals</subject><subject>Fossils</subject><subject>Geological time</subject><subject>Geology</subject><subject>Interspecific relationships</subject><subject>invertebrate</subject><subject>Invertebrates</subject><subject>Length</subject><subject>Lower Ordovician</subject><subject>Marine animals</subject><subject>Marine invertebrates</subject><subject>Marine organisms</subject><subject>Mineral nutrients</subject><subject>Morocco</subject><subject>North Africa</subject><subject>Nutrient availability</subject><subject>Nutrients</subject><subject>Ordovician</subject><subject>Original Article</subject><subject>Oxygenation</subject><subject>paleoenvironment</subject><subject>Paleontology</subject><subject>Paleozoic</subject><subject>Parameters</subject><subject>Platypeltoides</subject><subject>Predation</subject><subject>Predators</subject><subject>Sciences of the Universe</subject><subject>Sedimentary rocks</subject><subject>Shale</subject><subject>Shales</subject><subject>Storms</subject><subject>Stratigraphy</subject><subject>Trace fossils</subject><subject>Trilobita</subject><subject>Trilobitomorpha</subject><subject>Variation</subject><subject>Water 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trilobites in a stress-free Early Ordovician environment</title><author>Saleh, Farid ; Vidal, Muriel ; Laibl, Lukáš ; Sansjofre, Pierre ; Gueriau, Pierre ; Pérez-Peris, Francesc ; Lustri, Lorenzo ; Lucas, Victoire ; Lefebvre, Bertrand ; Pittet, Bernard ; El Hariri, Khadija ; Daley, Allison C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a501t-1207811d8dad5c54a25812e92bfa5202b0e490b847f78e185e83b1c2e52666423</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Abiotic factors</topic><topic>Adaptation</topic><topic>Africa</topic><topic>Arthropoda</topic><topic>biostratigraphy</topic><topic>Bioturbation</topic><topic>Body size</topic><topic>clastic rocks</topic><topic>Coring</topic><topic>depositional environment</topic><topic>Earth Sciences</topic><topic>Ecological adaptation</topic><topic>Environmental conditions</topic><topic>Fezouata Shale</topic><topic>Fossil 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Trilobite assemblages dominated by small- to normal-sized specimens that are a few centimetres in length are found in proximal and intermediate settings, while those comprising larger taxa more than 20 cm in length are found in the most distal environment of the Fezouata Shale. Drill core material from distal settings shows that sedimentary rocks hosting large trilobites preserved in situ are extensively bioturbated with a high diversity of trace fossils, indicating that oxygen and nutrients were available in this environment. In intermediate and shallow settings, bioturbation is less extensive and shallower in depth. The rarity of storm events (minimal physical disturbance) and the lack of predators in deep environments in comparison to shallower settings would also have helped trilobites attain larger body sizes. 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subjects | Abiotic factors Adaptation Africa Arthropoda biostratigraphy Bioturbation Body size clastic rocks Coring depositional environment Earth Sciences Ecological adaptation Environmental conditions Fezouata Shale Fossil animals Fossils Geological time Geology Interspecific relationships invertebrate Invertebrates Length Lower Ordovician Marine animals Marine invertebrates Marine organisms Mineral nutrients Morocco North Africa Nutrient availability Nutrients Ordovician Original Article Oxygenation paleoenvironment Paleontology Paleozoic Parameters Platypeltoides Predation Predators Sciences of the Universe Sedimentary rocks Shale Shales Storms Stratigraphy Trace fossils Trilobita Trilobitomorpha Variation Water temperature |
title | Large trilobites in a stress-free Early Ordovician environment |
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