6533b832fe1ef96bd1299f42
RESEARCH PRODUCT
Past aquatic environments in the Levant inferred from stable isotope compositions of carbonate and phosphate in fish teeth
Guy Sisma-venturaThomas TütkenStefan T. M. PetersOr M. BialikIrit ZoharAndreas Packsubject
Teeth550CarbonatesMarine and Aquatic SciencesOxygen IsotopesMedicine and Health SciencesChondrichthyesCarbon IsotopesQuaternary PeriodFossilsMediterranean RegionQREukaryotaGeologyBiological EvolutionFreshwater FishChemistryTeeth; Carbonates; Lagoons; Freshwater fish; Paleobiology; Holocene epoch; Sea water; Marine fishPhysical SciencesVertebratesMedicineAnatomyResearch ArticleLagoonsCarpsSciencePhosphatesSea WaterAnimalsEcosystemHolocene EpochEcology and Environmental SciencesChemical CompoundsOrganismsBiology and Life SciencesPaleontologyAquatic EnvironmentsGeologic TimeBodies of WaterMarine EnvironmentsCarbonSea BreamOxygenFishJawEarth SciencesSharksCenozoic EraPaleobiologyDigestive SystemHeadToothElasmobranchiidescription
Here we explore the carbon and oxygen isotope compositions of the co-existing carbonate and phosphate fractions of fish tooth enameloid as a tool to reconstruct past aquatic fish environments and harvesting grounds. The enameloid oxygen isotope compositions of the phosphate fraction (δ18OPO4) vary by as much as ~4‰ for migratory marine fish such as gilthead seabream (Sparus aurata), predominantly reflecting the different saline habitats it occupies during its life cycle. The offset in enameloid Δ18OCO3-PO4 values of modern marine Sparidae and freshwater Cyprinidae from the Southeast Mediterranean region vary between 8.1 and 11.0‰, similar to values reported for modern sharks. The mean δ13C of modern adult S. aurata and Cyprinus carpio teeth of 0.1±0.4‰ and -6.1±0.7‰, respectively, mainly reflect the difference in δ13C of dissolved inorganic carbon (DIC) of the ambient water and dietary carbon sources. The enameloid Δ18OCO3-PO4 and δ13C values of ancient S. aurata (Holocene) and fossil Luciobarbus sp. (Cyprinidae; mid Pleistocene) teeth agree well with those of modern specimens, implying little diagenetic alteration of these tooth samples. Paired δ18OPO4-δ13C data from ancient S. aurata teeth indicate that hypersaline water bodies formed in the Levant region during the Late Holocene from typical Mediterranean coastal water with high evaporation rates and limited carbon input from terrestrial sources. Sparid tooth stable isotopes further suggest that coastal lagoons in the Eastern Mediterranean had already formed by the Early Holocene and were influenced by terrestrial carbon sources. Overall, combined enameloid oxygen and carbon isotope analysis of fish teeth is a powerful tool to infer the hydrologic evolution of aquatic environments and assess past fishing grounds of human populations in antiquity. Open-Access-Publikationsfonds 2019 peerReviewed
year | journal | country | edition | language |
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2019-07-01 | PLOS ONE |