Changing diets over time: knock-on effects of marine megafauna overexploitation on their competitors in the southwestern Atlantic Ocean
This study compares the δ15N values and the trophic position of two seabird species throughout the late Holocene in three regions in the southwestern Atlantic Ocean to assess the hypothesis that the decimation of megafauna led to changes in the trophic position of mesopredators. Modern and ancient m...
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creator | Bas, Maria Tivoli, Angélica M. Godino, Ivan Briz i Salemme, Mónica Santiago, Fernando Belardi, Juan Bautista Borella, Florencia Vales, Damián G. Crespo, Enrique A. Cardona, Luis |
description | This study compares the δ15N values and the trophic position of two seabird species throughout the late Holocene in three regions in the southwestern Atlantic Ocean to assess the hypothesis that the decimation of megafauna led to changes in the trophic position of mesopredators. Modern and ancient mollusk shells were also analyzed to account for changes in the isotopic baseline through time. Results revealed that modern Magellanic penguins have higher δ15N values than their ancient conspecifics in the three regions, after controlling for changes in the isotopic baseline. This was also true for modern Imperial shags compared with ancient unidentified cormorants/shags from the two areas where ancient specimens were recovered (southern Patagonia and the Beagle Channel). Such temporal variability might be caused by three non–mutually exclusive processes: decreased availability of pelagic squat lobster resulting from decreasing primary productivity through the late Holocene, increased availability of small fishes resulting from the sequential depletion of other piscivores (South American fur seal and sea lion and Argentine hake) since the late eighteenth century, and modification of the migratory patterns of Magellanic penguins. Although disentangling the relative contribution of all those processes is impossible at this time, the results reported here demonstrate that the ecology of Magellanic penguins and Imperial shags has undergone major changes since the late Holocene. |
doi_str_mv | 10.1017/pab.2022.19 |
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Modern and ancient mollusk shells were also analyzed to account for changes in the isotopic baseline through time. Results revealed that modern Magellanic penguins have higher δ15N values than their ancient conspecifics in the three regions, after controlling for changes in the isotopic baseline. This was also true for modern Imperial shags compared with ancient unidentified cormorants/shags from the two areas where ancient specimens were recovered (southern Patagonia and the Beagle Channel). Such temporal variability might be caused by three non–mutually exclusive processes: decreased availability of pelagic squat lobster resulting from decreasing primary productivity through the late Holocene, increased availability of small fishes resulting from the sequential depletion of other piscivores (South American fur seal and sea lion and Argentine hake) since the late eighteenth century, and modification of the migratory patterns of Magellanic penguins. Although disentangling the relative contribution of all those processes is impossible at this time, the results reported here demonstrate that the ecology of Magellanic penguins and Imperial shags has undergone major changes since the late Holocene.</description><identifier>ISSN: 0094-8373</identifier><identifier>EISSN: 1938-5331</identifier><identifier>DOI: 10.1017/pab.2022.19</identifier><language>eng</language><publisher>New York, USA: The Paleontological Society</publisher><subject>Aptenodytes ; Aptenodytes patagonicus ; Aquatic birds ; Aquatic mammals ; Arctocephalus australis ; Argentina ; Atlantic Ocean ; Aulacomya atra ; Availability ; Aves ; Birds ; Bivalvia ; Bones ; Cenozoic ; chemical composition ; Chordata ; Chubut Argentina ; Coasts ; Competitors ; Conspecifics ; Crustaceans ; Depletion ; diet ; Ecological effects ; Fish ; Fishing ; Geochemistry ; Historic buildings & sites ; Holocene ; human activity ; isotope ratios ; Isotopes ; Leucocarbo ; Leucocarbo atriceps ; Marine crustaceans ; marine environment ; Marine fishes ; Marine mammals ; Megafauna ; Merluccius hubbsi ; Mollusca ; Mollusks ; Mytilus ; Mytilus chilensis ; N-15/N-14 ; Nacella magellanica ; Neognathae ; Neornithes ; nitrogen ; Overexploitation ; paleoecology ; paleoenvironment ; Paleontology ; Patagonia ; Phalacrocorax ; Piscivores ; Primary production ; Quaternary ; Ratios ; Reference materials ; Rio Negro Argentina ; Santa Cruz Argentina ; Seabirds ; Shellfish ; Shells ; South America ; South Atlantic ; Southwest Atlantic ; Sphenisciformes ; Spheniscus magellanicus ; stable isotopes ; statistical analysis ; Temporal variations ; Tetrapoda ; Tierra del Fuego ; upper Holocene ; Vertebrata ; vertebrate</subject><ispartof>Paleobiology, 2023-02, Vol.49 (1), p.176-190</ispartof><rights>Copyright © The Author(s), 2022. Published by Cambridge University Press on behalf of The Paleontological Society</rights><rights>GeoRef, Copyright 2023, American Geosciences Institute. Reference includes data from GeoScienceWorld @Alexandria, VA @USA @United States. Abstract, Copyright, The Paleontological Society</rights><rights>Copyright © The Author(s), 2022. Published by Cambridge University Press on behalf of The Paleontological Society. This work is licensed under the Creative Commons Attribution License https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a387t-633f0a0102da6557fd08e3f2391d46d7511437f28fd08a592dca49c27c8a9d7f3</cites><orcidid>0000-0001-8553-6557</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0094837322000197/type/journal_article$$EHTML$$P50$$Gcambridge$$Hfree_for_read</linktohtml><link.rule.ids>164,314,780,784,27924,27925,55628</link.rule.ids></links><search><creatorcontrib>Bas, Maria</creatorcontrib><creatorcontrib>Tivoli, Angélica M.</creatorcontrib><creatorcontrib>Godino, Ivan Briz i</creatorcontrib><creatorcontrib>Salemme, Mónica</creatorcontrib><creatorcontrib>Santiago, Fernando</creatorcontrib><creatorcontrib>Belardi, Juan Bautista</creatorcontrib><creatorcontrib>Borella, Florencia</creatorcontrib><creatorcontrib>Vales, Damián G.</creatorcontrib><creatorcontrib>Crespo, Enrique A.</creatorcontrib><creatorcontrib>Cardona, Luis</creatorcontrib><title>Changing diets over time: knock-on effects of marine megafauna overexploitation on their competitors in the southwestern Atlantic Ocean</title><title>Paleobiology</title><addtitle>Paleobiology</addtitle><description>This study compares the δ15N values and the trophic position of two seabird species throughout the late Holocene in three regions in the southwestern Atlantic Ocean to assess the hypothesis that the decimation of megafauna led to changes in the trophic position of mesopredators. Modern and ancient mollusk shells were also analyzed to account for changes in the isotopic baseline through time. Results revealed that modern Magellanic penguins have higher δ15N values than their ancient conspecifics in the three regions, after controlling for changes in the isotopic baseline. This was also true for modern Imperial shags compared with ancient unidentified cormorants/shags from the two areas where ancient specimens were recovered (southern Patagonia and the Beagle Channel). Such temporal variability might be caused by three non–mutually exclusive processes: decreased availability of pelagic squat lobster resulting from decreasing primary productivity through the late Holocene, increased availability of small fishes resulting from the sequential depletion of other piscivores (South American fur seal and sea lion and Argentine hake) since the late eighteenth century, and modification of the migratory patterns of Magellanic penguins. Although disentangling the relative contribution of all those processes is impossible at this time, the results reported here demonstrate that the ecology of Magellanic penguins and Imperial shags has undergone major changes since the late Holocene.</description><subject>Aptenodytes</subject><subject>Aptenodytes patagonicus</subject><subject>Aquatic birds</subject><subject>Aquatic mammals</subject><subject>Arctocephalus australis</subject><subject>Argentina</subject><subject>Atlantic Ocean</subject><subject>Aulacomya atra</subject><subject>Availability</subject><subject>Aves</subject><subject>Birds</subject><subject>Bivalvia</subject><subject>Bones</subject><subject>Cenozoic</subject><subject>chemical composition</subject><subject>Chordata</subject><subject>Chubut Argentina</subject><subject>Coasts</subject><subject>Competitors</subject><subject>Conspecifics</subject><subject>Crustaceans</subject><subject>Depletion</subject><subject>diet</subject><subject>Ecological effects</subject><subject>Fish</subject><subject>Fishing</subject><subject>Geochemistry</subject><subject>Historic buildings & sites</subject><subject>Holocene</subject><subject>human activity</subject><subject>isotope ratios</subject><subject>Isotopes</subject><subject>Leucocarbo</subject><subject>Leucocarbo atriceps</subject><subject>Marine crustaceans</subject><subject>marine environment</subject><subject>Marine fishes</subject><subject>Marine mammals</subject><subject>Megafauna</subject><subject>Merluccius hubbsi</subject><subject>Mollusca</subject><subject>Mollusks</subject><subject>Mytilus</subject><subject>Mytilus chilensis</subject><subject>N-15/N-14</subject><subject>Nacella magellanica</subject><subject>Neognathae</subject><subject>Neornithes</subject><subject>nitrogen</subject><subject>Overexploitation</subject><subject>paleoecology</subject><subject>paleoenvironment</subject><subject>Paleontology</subject><subject>Patagonia</subject><subject>Phalacrocorax</subject><subject>Piscivores</subject><subject>Primary production</subject><subject>Quaternary</subject><subject>Ratios</subject><subject>Reference materials</subject><subject>Rio Negro Argentina</subject><subject>Santa Cruz Argentina</subject><subject>Seabirds</subject><subject>Shellfish</subject><subject>Shells</subject><subject>South America</subject><subject>South Atlantic</subject><subject>Southwest Atlantic</subject><subject>Sphenisciformes</subject><subject>Spheniscus magellanicus</subject><subject>stable isotopes</subject><subject>statistical analysis</subject><subject>Temporal variations</subject><subject>Tetrapoda</subject><subject>Tierra del Fuego</subject><subject>upper 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megafauna overexploitation on their competitors in the southwestern Atlantic Ocean</title><author>Bas, Maria ; Tivoli, Angélica M. ; Godino, Ivan Briz i ; Salemme, Mónica ; Santiago, Fernando ; Belardi, Juan Bautista ; Borella, Florencia ; Vales, Damián G. ; Crespo, Enrique A. ; Cardona, Luis</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a387t-633f0a0102da6557fd08e3f2391d46d7511437f28fd08a592dca49c27c8a9d7f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Aptenodytes</topic><topic>Aptenodytes patagonicus</topic><topic>Aquatic birds</topic><topic>Aquatic mammals</topic><topic>Arctocephalus australis</topic><topic>Argentina</topic><topic>Atlantic Ocean</topic><topic>Aulacomya atra</topic><topic>Availability</topic><topic>Aves</topic><topic>Birds</topic><topic>Bivalvia</topic><topic>Bones</topic><topic>Cenozoic</topic><topic>chemical 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Modern and ancient mollusk shells were also analyzed to account for changes in the isotopic baseline through time. Results revealed that modern Magellanic penguins have higher δ15N values than their ancient conspecifics in the three regions, after controlling for changes in the isotopic baseline. This was also true for modern Imperial shags compared with ancient unidentified cormorants/shags from the two areas where ancient specimens were recovered (southern Patagonia and the Beagle Channel). Such temporal variability might be caused by three non–mutually exclusive processes: decreased availability of pelagic squat lobster resulting from decreasing primary productivity through the late Holocene, increased availability of small fishes resulting from the sequential depletion of other piscivores (South American fur seal and sea lion and Argentine hake) since the late eighteenth century, and modification of the migratory patterns of Magellanic penguins. 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subjects | Aptenodytes Aptenodytes patagonicus Aquatic birds Aquatic mammals Arctocephalus australis Argentina Atlantic Ocean Aulacomya atra Availability Aves Birds Bivalvia Bones Cenozoic chemical composition Chordata Chubut Argentina Coasts Competitors Conspecifics Crustaceans Depletion diet Ecological effects Fish Fishing Geochemistry Historic buildings & sites Holocene human activity isotope ratios Isotopes Leucocarbo Leucocarbo atriceps Marine crustaceans marine environment Marine fishes Marine mammals Megafauna Merluccius hubbsi Mollusca Mollusks Mytilus Mytilus chilensis N-15/N-14 Nacella magellanica Neognathae Neornithes nitrogen Overexploitation paleoecology paleoenvironment Paleontology Patagonia Phalacrocorax Piscivores Primary production Quaternary Ratios Reference materials Rio Negro Argentina Santa Cruz Argentina Seabirds Shellfish Shells South America South Atlantic Southwest Atlantic Sphenisciformes Spheniscus magellanicus stable isotopes statistical analysis Temporal variations Tetrapoda Tierra del Fuego upper Holocene Vertebrata vertebrate |
title | Changing diets over time: knock-on effects of marine megafauna overexploitation on their competitors in the southwestern Atlantic Ocean |
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