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Shell sclerochronology and stable isotopes of the bivalve Anomalocardia flexuosa (Linnaeus, 1767) from southern Brazil: implications for environmental and archaeological studies

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Author(s)

  • Andre Carlo Colonese
  • Sérgio Antônio Netto
  • André Silva Francisco
  • Paulo DeBlasis
  • Ximena S. Villagran
  • Raquel De Almeida Rocha Ponzoni
  • Yvette Hancock
  • Niklas Hausmann
  • Deisi Sunderlick Faria
  • Amy Prendergast
  • Bernd R. Schöne
  • Francisco William da Cruz Junior
  • Paulo César Fonseca Giannini

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Publication details

JournalPalaeogeography palaeoclimatology palaeoecology
DateAccepted/In press - 4 Jan 2017
DateE-pub ahead of print - 6 Jan 2017
DatePublished (current) - 15 Oct 2017
Number of pages15
Pages (from-to)1-15
Early online date6/01/17
Original languageEnglish

Abstract

We conduct 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). As shells of Anomalocardia flexuosa are also the main components of pre-Columbian archaeological shell mounds and middens distributed along the Brazilian coastline, late Holocene archaeological specimens from a local shell mound (Cabeçuda) were selected to compare their stable carbon and oxygen isotopes 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 Cabeçuda 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.

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