First stable isotope results on the ecology of the straight-tusked elephant (Palaeoloxodon antiquus) from the Middle Pleistocene Marathousa 1 (Peloponnese, Greece)

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dc.contributor.author Roditi, Effrosyni
dc.contributor.author Bocherens, Herve
dc.contributor.author Konidaris, George
dc.contributor.author Athanassiou, Athanassios
dc.contributor.author Tourloukis, Vangelis
dc.contributor.author Panagopoulou, Eleni
dc.contributor.author Harvati, Katerina
dc.date.accessioned 2024-08-08T08:49:04Z
dc.date.available 2024-08-08T08:49:04Z
dc.date.issued 2024
dc.identifier.isbn 978-3-98945-002-8
dc.identifier.uri http://hdl.handle.net/10900/156338
dc.identifier.uri http://nbn-resolving.de/urn:nbn:de:bsz:21-dspace-1563387 de_DE
dc.identifier.uri http://dx.doi.org/10.15496/publikation-97670
dc.description.abstract Carbon and oxygen stable isotope analysis of mammalian carbonate bioapatite is, nowadays, a well-established and widely used approach for past ecological investigations and paleoenvironmental reconstructions. Carbon is incorporated into mammalian tissues through their dietary intake. In this regard, the ratios of stable carbon isotopes in the tissues of primary consumers—hereafter expressed using the delta (δ) notation, wherein δ13C=[(13C/12C)sample/(13C/12C)standard – 1] × 1000— reflect the isotopic composition of the ingested plant matter (DeNiro and Epstein, 1978), enriched by ~14.1 ± 0.5‰ in tooth enamel carbonate of large herbivores (Cerling and Harris, 1999; Passey et al., 2005), due to physiological and metabolic processes. In terrestrial ecosystems, variation in the isotopic signature of plant carbon permits a distinction between the two main photosynthetic pathways, i.e., C4 and C3 (Ehleringer and Monson, 1993), with the former group consisting of warm growth season grasses and forbs, which demonstrate higher average δ13C value (~13‰), and the latter incorporating trees, shrubs, and cool growth season grasses and sedges with a modern average δ13C value of ~27‰ (Bender, 1971; Kohn, 2010). Within plant communities utilizing the C3 photosynthetic pathway, additional environmentally controlled fractionation occurs, which is governed by multiple factors, such as degree of canopy closure, water availability, temperature, irradiance, or atmospheric CO2 diffusion (van der Merwe and Medina, 1991; Heaton, 1999; Hofman-Kamińska et al., 2018). The interplay of these factors enables further habitat distinctions within the wide range of δ13C values documented in C3-dominated ecosystems, since carbon isotopic ratios of herbivores feeding under closed canopy conditions, i.e., dense forests, tend to be lower than for herbivores foraging in open woodlands, open parklands and grasslands, or at the top of the canopy (Drucker et al., 2008; Bocherens and Drucker, 2013). en
dc.language.iso en de_DE
dc.publisher Tübingen University Press de_DE
dc.subject.classification Stabiles Isotop , Palökologie de_DE
dc.subject.ddc 930 de_DE
dc.subject.other Stable isotopes en
dc.subject.other paleoecology en
dc.subject.other Middle Pleistocene en
dc.subject.other Palaeoloxodon en
dc.subject.other Megalopolis Basin en
dc.title First stable isotope results on the ecology of the straight-tusked elephant (Palaeoloxodon antiquus) from the Middle Pleistocene Marathousa 1 (Peloponnese, Greece) en
dc.type BookPart de_DE
utue.publikation.fachbereich Geographie, Geoökologie, Geowissenschaft de_DE
utue.publikation.fakultaet 7 Mathematisch-Naturwissenschaftliche Fakultät de_DE
utue.opus.portal tpbs3 de_DE
utue.publikation.noppn yes de_DE


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