Dietary and paleoenvironmental reconstruction using stable isotopes of herbivore tooth enamel from middle Pliocene Dikika, Ethiopia: Implication for Australopithecus afarensis habitat and food resources
Carbon and oxygen isotopes of mammalian tooth enamel were used to reconstruct paleoenvironments of Australopithecus afarensis from the middle Pliocene locality of Dikika, Ethiopia. Isotopic analyses were conducted on 210 mammalian herbivore teeth from 15 different taxa collected from the Basal Membe...
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description | Carbon and oxygen isotopes of mammalian tooth enamel were used to reconstruct paleoenvironments of Australopithecus afarensis from the middle Pliocene locality of Dikika, Ethiopia. Isotopic analyses were conducted on 210 mammalian herbivore teeth from 15 different taxa collected from the Basal Member (∼3.8–3.42 Ma) and Sidi Hakoma Member (3.42–3.24 Ma) of the Hadar Formation. The isotopic analyses aim specifically at reconstructing shifts in the relative abundance of C4 grasses in mammalian diets, and more generally at paleoclimate factors such as aridity and seasonality, as well as habitat structure. Carbon isotopic data suggest a wide range of foraging strategies, characterized by mixed C3/C4 to C4-dominated diets in wooded grasslands to open woodlands. Weighted average C4 dietary proportions range between 60% and 86% in the Basal Member and 49% and 74% in the Sidi Hakoma Member. Paleoclimatic conditions based on the reconstructed mean annual water deficit from the δ18Oenamel values indicate a wetter climate as compared to either the early Pliocene or the Pleistocene nearby. The middle Pliocene habitat structure at Dikika could be as diverse as open grassland and wooded grassland, and woodland to forest in the Sidi Hakoma Member while wooded grassland, woodland to grassland are evident in the Basal Member. All habitats except closed woodland and forest are persistent through both members; however, the relative proportion of individual habitats changed through time. These changes could have put the fauna in competition for preferred habitats and food resources, which could have forced migration, adaptation to other resources and/or extinction. Thus, the existence of A. afarensis throughout the middle Pliocene indicates either this species might have adapted to a wide range of habitats, or its preferred habitat was not affected by the observed environmental changes. |
doi_str_mv | 10.1016/j.jhevol.2012.05.015 |
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Isotopic analyses were conducted on 210 mammalian herbivore teeth from 15 different taxa collected from the Basal Member (∼3.8–3.42 Ma) and Sidi Hakoma Member (3.42–3.24 Ma) of the Hadar Formation. The isotopic analyses aim specifically at reconstructing shifts in the relative abundance of C4 grasses in mammalian diets, and more generally at paleoclimate factors such as aridity and seasonality, as well as habitat structure. Carbon isotopic data suggest a wide range of foraging strategies, characterized by mixed C3/C4 to C4-dominated diets in wooded grasslands to open woodlands. Weighted average C4 dietary proportions range between 60% and 86% in the Basal Member and 49% and 74% in the Sidi Hakoma Member. Paleoclimatic conditions based on the reconstructed mean annual water deficit from the δ18Oenamel values indicate a wetter climate as compared to either the early Pliocene or the Pleistocene nearby. The middle Pliocene habitat structure at Dikika could be as diverse as open grassland and wooded grassland, and woodland to forest in the Sidi Hakoma Member while wooded grassland, woodland to grassland are evident in the Basal Member. All habitats except closed woodland and forest are persistent through both members; however, the relative proportion of individual habitats changed through time. These changes could have put the fauna in competition for preferred habitats and food resources, which could have forced migration, adaptation to other resources and/or extinction. Thus, the existence of A. afarensis throughout the middle Pliocene indicates either this species might have adapted to a wide range of habitats, or its preferred habitat was not affected by the observed environmental changes.</description><identifier>ISSN: 0047-2484</identifier><identifier>EISSN: 1095-8606</identifier><identifier>DOI: 10.1016/j.jhevol.2012.05.015</identifier><identifier>PMID: 23199576</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>Abundance ; Adaptations ; Africa ; Animals ; Anthropology, Physical ; Australopithecines ; Australopithecus afarensis ; Carbon ; Carbon Isotopes - analysis ; Climate ; Competition ; Data processing ; Dental enamel ; Dental Enamel - chemistry ; Diet ; Diets ; Dikika ; Environment ; Environmental changes ; Environmental studies ; Ethiopia ; Extinction ; Food resources ; Foraging behavior ; Forests ; Fossils ; Grasses ; Grasslands ; Habitat ; Herbivores ; Hominidae - anatomy & histology ; Hominidae - physiology ; Human paleontology ; Isotopes ; Mammals ; Methodology and general studies ; Middle Pliocene ; Migration ; Oxygen ; Oxygen Isotopes - analysis ; Palaeolithic and epipalaeolithic ; Paleoanthropology ; Paleoclimatology ; Paleoecology ; Paleoenvironments ; Pliocene ; Prehistory and protohistory ; Seasonal variations ; Southern and East Africa ; Stable isotope ; Teeth ; Tooth - chemistry ; Tooth enamel</subject><ispartof>Journal of human evolution, 2013-01, Vol.64 (1), p.21-38</ispartof><rights>2012 Elsevier Ltd</rights><rights>2015 INIST-CNRS</rights><rights>Copyright © 2012 Elsevier Ltd. All rights reserved.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c492t-b68839781f225c7ce5f9ec9e13cfcc2103f6d31171af6835aa416a30d4b4670a3</citedby><cites>FETCH-LOGICAL-c492t-b68839781f225c7ce5f9ec9e13cfcc2103f6d31171af6835aa416a30d4b4670a3</cites><orcidid>0000-0003-2475-8011</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.jhevol.2012.05.015$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,315,782,786,887,3554,4028,27932,27933,27934,46004</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=27104975$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/23199576$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-00807902$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Bedaso, Zelalem K.</creatorcontrib><creatorcontrib>Wynn, Jonathan G.</creatorcontrib><creatorcontrib>Alemseged, Zeresenay</creatorcontrib><creatorcontrib>Geraads, Denis</creatorcontrib><title>Dietary and paleoenvironmental reconstruction using stable isotopes of herbivore tooth enamel from middle Pliocene Dikika, Ethiopia: Implication for Australopithecus afarensis habitat and food resources</title><title>Journal of human evolution</title><addtitle>J Hum Evol</addtitle><description>Carbon and oxygen isotopes of mammalian tooth enamel were used to reconstruct paleoenvironments of Australopithecus afarensis from the middle Pliocene locality of Dikika, Ethiopia. Isotopic analyses were conducted on 210 mammalian herbivore teeth from 15 different taxa collected from the Basal Member (∼3.8–3.42 Ma) and Sidi Hakoma Member (3.42–3.24 Ma) of the Hadar Formation. The isotopic analyses aim specifically at reconstructing shifts in the relative abundance of C4 grasses in mammalian diets, and more generally at paleoclimate factors such as aridity and seasonality, as well as habitat structure. Carbon isotopic data suggest a wide range of foraging strategies, characterized by mixed C3/C4 to C4-dominated diets in wooded grasslands to open woodlands. Weighted average C4 dietary proportions range between 60% and 86% in the Basal Member and 49% and 74% in the Sidi Hakoma Member. Paleoclimatic conditions based on the reconstructed mean annual water deficit from the δ18Oenamel values indicate a wetter climate as compared to either the early Pliocene or the Pleistocene nearby. The middle Pliocene habitat structure at Dikika could be as diverse as open grassland and wooded grassland, and woodland to forest in the Sidi Hakoma Member while wooded grassland, woodland to grassland are evident in the Basal Member. All habitats except closed woodland and forest are persistent through both members; however, the relative proportion of individual habitats changed through time. These changes could have put the fauna in competition for preferred habitats and food resources, which could have forced migration, adaptation to other resources and/or extinction. Thus, the existence of A. afarensis throughout the middle Pliocene indicates either this species might have adapted to a wide range of habitats, or its preferred habitat was not affected by the observed environmental changes.</description><subject>Abundance</subject><subject>Adaptations</subject><subject>Africa</subject><subject>Animals</subject><subject>Anthropology, Physical</subject><subject>Australopithecines</subject><subject>Australopithecus afarensis</subject><subject>Carbon</subject><subject>Carbon Isotopes - analysis</subject><subject>Climate</subject><subject>Competition</subject><subject>Data processing</subject><subject>Dental enamel</subject><subject>Dental Enamel - chemistry</subject><subject>Diet</subject><subject>Diets</subject><subject>Dikika</subject><subject>Environment</subject><subject>Environmental changes</subject><subject>Environmental studies</subject><subject>Ethiopia</subject><subject>Extinction</subject><subject>Food resources</subject><subject>Foraging behavior</subject><subject>Forests</subject><subject>Fossils</subject><subject>Grasses</subject><subject>Grasslands</subject><subject>Habitat</subject><subject>Herbivores</subject><subject>Hominidae - anatomy & histology</subject><subject>Hominidae - physiology</subject><subject>Human paleontology</subject><subject>Isotopes</subject><subject>Mammals</subject><subject>Methodology and general studies</subject><subject>Middle Pliocene</subject><subject>Migration</subject><subject>Oxygen</subject><subject>Oxygen Isotopes - analysis</subject><subject>Palaeolithic and epipalaeolithic</subject><subject>Paleoanthropology</subject><subject>Paleoclimatology</subject><subject>Paleoecology</subject><subject>Paleoenvironments</subject><subject>Pliocene</subject><subject>Prehistory and protohistory</subject><subject>Seasonal variations</subject><subject>Southern and East Africa</subject><subject>Stable isotope</subject><subject>Teeth</subject><subject>Tooth - chemistry</subject><subject>Tooth enamel</subject><issn>0047-2484</issn><issn>1095-8606</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNqNkk2LFDEQhhtR3HH1H4jkIig4Yz7604Mw7K7uwoAe9Byq0xU7s-lkTNID_kV_lZmdcb2pp0DyVNVL6imK54yuGGX12-1qO-Le2xWnjK9otaKselAsGO2qZVvT-mGxoLRslrxsy7PiSYxbSmlXCv64OOOCdV3V1Ivi56XBBOEHATeQHVj06PYmeDehS2BJQOVdTGFWyXhH5mjcNxIT9BaJiT75HUbiNRkx9GbvA5LkfRoJOpjQEh38RCYzDBn_bI1X6JBcmltzC2_IVRqN3xl4R26mnTUK7kZoH8h6ziPB5sc0opojAQ0BXTSRjNCbBOkur_Z-yAmjn4PC-LR4pMFGfHY6z4uvH66-XFwvN58-3lysN0tVdjwt-7ptRde0THNeqUZhpTtUHTKhtFKcUaHrQTDWMNB1KyqAktUg6FD2Zd1QEOfF62PfEazcBTPl75MejLxeb-ThjtKWNh3le5bZV0d2F_z3GWOSk4kKrQWHfo6S5UXUjNW0_TfKG1EKwZvuf9ADzCue0fKIquBjDKjvEzMqDx7JrTx6JA8eSVrJ7FEue3GaMPcTDvdFv8XJwMsTAFGB1QGcMvEP1zBads2h0fsjh3kje4NBRmXQKRxMVivJwZu_J_kFDHPsHA</recordid><startdate>201301</startdate><enddate>201301</enddate><creator>Bedaso, Zelalem K.</creator><creator>Wynn, Jonathan G.</creator><creator>Alemseged, Zeresenay</creator><creator>Geraads, Denis</creator><general>Elsevier Ltd</general><general>Elsevier</general><general>Elsevier [1972-....]</general><scope>IQODW</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QP</scope><scope>7SN</scope><scope>7ST</scope><scope>7U6</scope><scope>C1K</scope><scope>7X8</scope><scope>8BJ</scope><scope>FQK</scope><scope>JBE</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0003-2475-8011</orcidid></search><sort><creationdate>201301</creationdate><title>Dietary and paleoenvironmental reconstruction using stable isotopes of herbivore tooth enamel from middle Pliocene Dikika, Ethiopia: Implication for Australopithecus afarensis habitat and food resources</title><author>Bedaso, Zelalem K. ; Wynn, Jonathan G. ; Alemseged, Zeresenay ; Geraads, Denis</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c492t-b68839781f225c7ce5f9ec9e13cfcc2103f6d31171af6835aa416a30d4b4670a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Abundance</topic><topic>Adaptations</topic><topic>Africa</topic><topic>Animals</topic><topic>Anthropology, Physical</topic><topic>Australopithecines</topic><topic>Australopithecus afarensis</topic><topic>Carbon</topic><topic>Carbon Isotopes - analysis</topic><topic>Climate</topic><topic>Competition</topic><topic>Data processing</topic><topic>Dental enamel</topic><topic>Dental Enamel - chemistry</topic><topic>Diet</topic><topic>Diets</topic><topic>Dikika</topic><topic>Environment</topic><topic>Environmental changes</topic><topic>Environmental studies</topic><topic>Ethiopia</topic><topic>Extinction</topic><topic>Food resources</topic><topic>Foraging behavior</topic><topic>Forests</topic><topic>Fossils</topic><topic>Grasses</topic><topic>Grasslands</topic><topic>Habitat</topic><topic>Herbivores</topic><topic>Hominidae - anatomy & histology</topic><topic>Hominidae - physiology</topic><topic>Human paleontology</topic><topic>Isotopes</topic><topic>Mammals</topic><topic>Methodology and general studies</topic><topic>Middle Pliocene</topic><topic>Migration</topic><topic>Oxygen</topic><topic>Oxygen Isotopes - analysis</topic><topic>Palaeolithic and epipalaeolithic</topic><topic>Paleoanthropology</topic><topic>Paleoclimatology</topic><topic>Paleoecology</topic><topic>Paleoenvironments</topic><topic>Pliocene</topic><topic>Prehistory and protohistory</topic><topic>Seasonal variations</topic><topic>Southern and East Africa</topic><topic>Stable isotope</topic><topic>Teeth</topic><topic>Tooth - chemistry</topic><topic>Tooth enamel</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bedaso, Zelalem K.</creatorcontrib><creatorcontrib>Wynn, Jonathan G.</creatorcontrib><creatorcontrib>Alemseged, Zeresenay</creatorcontrib><creatorcontrib>Geraads, Denis</creatorcontrib><collection>Pascal-Francis</collection><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Calcium & Calcified Tissue Abstracts</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>MEDLINE - Academic</collection><collection>International Bibliography of the Social Sciences (IBSS)</collection><collection>International Bibliography of the Social Sciences</collection><collection>International Bibliography of the Social Sciences</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Journal of human evolution</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bedaso, Zelalem K.</au><au>Wynn, Jonathan G.</au><au>Alemseged, Zeresenay</au><au>Geraads, Denis</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dietary and paleoenvironmental reconstruction using stable isotopes of herbivore tooth enamel from middle Pliocene Dikika, Ethiopia: Implication for Australopithecus afarensis habitat and food resources</atitle><jtitle>Journal of human evolution</jtitle><addtitle>J Hum Evol</addtitle><date>2013-01</date><risdate>2013</risdate><volume>64</volume><issue>1</issue><spage>21</spage><epage>38</epage><pages>21-38</pages><issn>0047-2484</issn><eissn>1095-8606</eissn><abstract>Carbon and oxygen isotopes of mammalian tooth enamel were used to reconstruct paleoenvironments of Australopithecus afarensis from the middle Pliocene locality of Dikika, Ethiopia. Isotopic analyses were conducted on 210 mammalian herbivore teeth from 15 different taxa collected from the Basal Member (∼3.8–3.42 Ma) and Sidi Hakoma Member (3.42–3.24 Ma) of the Hadar Formation. The isotopic analyses aim specifically at reconstructing shifts in the relative abundance of C4 grasses in mammalian diets, and more generally at paleoclimate factors such as aridity and seasonality, as well as habitat structure. Carbon isotopic data suggest a wide range of foraging strategies, characterized by mixed C3/C4 to C4-dominated diets in wooded grasslands to open woodlands. Weighted average C4 dietary proportions range between 60% and 86% in the Basal Member and 49% and 74% in the Sidi Hakoma Member. Paleoclimatic conditions based on the reconstructed mean annual water deficit from the δ18Oenamel values indicate a wetter climate as compared to either the early Pliocene or the Pleistocene nearby. The middle Pliocene habitat structure at Dikika could be as diverse as open grassland and wooded grassland, and woodland to forest in the Sidi Hakoma Member while wooded grassland, woodland to grassland are evident in the Basal Member. All habitats except closed woodland and forest are persistent through both members; however, the relative proportion of individual habitats changed through time. These changes could have put the fauna in competition for preferred habitats and food resources, which could have forced migration, adaptation to other resources and/or extinction. Thus, the existence of A. afarensis throughout the middle Pliocene indicates either this species might have adapted to a wide range of habitats, or its preferred habitat was not affected by the observed environmental changes.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><pmid>23199576</pmid><doi>10.1016/j.jhevol.2012.05.015</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0003-2475-8011</orcidid></addata></record> |
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subjects | Abundance Adaptations Africa Animals Anthropology, Physical Australopithecines Australopithecus afarensis Carbon Carbon Isotopes - analysis Climate Competition Data processing Dental enamel Dental Enamel - chemistry Diet Diets Dikika Environment Environmental changes Environmental studies Ethiopia Extinction Food resources Foraging behavior Forests Fossils Grasses Grasslands Habitat Herbivores Hominidae - anatomy & histology Hominidae - physiology Human paleontology Isotopes Mammals Methodology and general studies Middle Pliocene Migration Oxygen Oxygen Isotopes - analysis Palaeolithic and epipalaeolithic Paleoanthropology Paleoclimatology Paleoecology Paleoenvironments Pliocene Prehistory and protohistory Seasonal variations Southern and East Africa Stable isotope Teeth Tooth - chemistry Tooth enamel |
title | Dietary and paleoenvironmental reconstruction using stable isotopes of herbivore tooth enamel from middle Pliocene Dikika, Ethiopia: Implication for Australopithecus afarensis habitat and food resources |
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