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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Veröffentlicht in:Journal of human evolution 2013-01, Vol.64 (1), p.21-38
Hauptverfasser: Bedaso, Zelalem K., Wynn, Jonathan G., Alemseged, Zeresenay, Geraads, Denis
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creator Bedaso, Zelalem K.
Wynn, Jonathan G.
Alemseged, Zeresenay
Geraads, Denis
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.
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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. 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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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