6533b857fe1ef96bd12b4636
RESEARCH PRODUCT
Shell sclerochronology and stable isotopes of the bivalve Anomalocardia flexuosa (Linnaeus, 1767) from southern Brazil: Implications for environmental and archaeological studies
Ximena S. VillagranPaulo César Fonseca GianniniDeisi Sunderlick Eloy De FariasNiklas HausmannNiklas HausmannSérgio Antônio NettoBernd R. SchöneAndré Silva FranciscoPaulo DeblasisAmy L. PrendergastY. HancockFrancisco W. CruzRaquel De Almeida Rocha PonzoniAndré Carlo Colonesesubject
010506 paleontology010504 meteorology & atmospheric sciencesδ13Cδ18OStable isotope ratioPaleontologySubtropicsOceanography01 natural sciencesArchaeologyIsotopes of oxygenMiddenSclerochronologyISÓTOPOS ESTÁVEISEcology Evolution Behavior and SystematicsGeologyHolocene0105 earth and related environmental sciencesEarth-Surface Processesdescription
Abstract This study presents the first stable isotopic and sclerochronological calibration of the bivalve Anomalocardia flexuosa (Linnaeus, 1767) in relation to environmental variables in a subtropical coastal area of southern Brazil. We investigate incremental shell growth patterns and δ18O and δ13C values of modern specimens collected alive from the Laguna Lagoonal System (LLS). Shells of Anomalocardia flexuosa are also one of the main biological components of pre-Columbian archaeological shell mounds and middens distributed along the Brazilian coastline. We therefore selected archaeological specimens from a local late Holocene shell mound (Cabecuda) to compare their stable carbon and oxygen isotope values with those of modern specimens. Shell growth increments, δ18O and δ13C values respond to a complex of environmental conditions, involving, for example, the effects of temperature and salinity. The isotopic information extracted from archaeological specimens from Cabecuda shell midden in the LLS indirectly indicates that environmental conditions during the late Holocene were different from present day. In particular, intra-shell δ18O and δ13C values of archaeological shells reveal a stronger marine influence at 3 ka cal BP, which is in contrast to the seasonal freshwater/seawater balance that currently prevails at the LLS.
year | journal | country | edition | language |
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2017-10-01 | Palaeogeography, Palaeoclimatology, Palaeoecology |