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STABLE ISOTOPIC ANALYSIS AND RADIOCARBON DATING OF MICROPOGONIAS FURNIERI OTOLITHS (SCIAENIDAE) FROM SOUTHEASTERN BRAZILIAN COAST: SEASONAL PALAEOENVIRONMENTAL INSIGHT

Published online by Cambridge University Press:  12 September 2022

Mariana Samor Lopes Open the ORCID record for Mariana Samor Lopes [Opens in a new window] ,
Elise Dufour Open the ORCID record for Elise Dufour [Opens in a new window] ,
Elisamara Sabadini-Santos Open the ORCID record for Elisamara Sabadini-Santos [Opens in a new window] ,
Maria Dulce Gaspar Open the ORCID record for Maria Dulce Gaspar [Opens in a new window] ,
Kita Macario Open the ORCID record for Kita Macario [Opens in a new window] ,
Bruna da Silva Mota Neto ,
Olivier Tombret ,
Denis Fiorillo ,
Michel Lemoine  and
Leandro Amaro Pessoa
...Show all authors
Mariana Samor Lopes*
Affiliation:
Departamento de Biologia Marinha, Universidade Federal Fluminense (UFF), Laboratório de Paleoecologia e Mudanças Globais (LP&MG). Campus Gragoatá, Bloco M, 24210-201, Niterói, RJ, Brazil
Elise Dufour
Affiliation:
Archéozoologie, Archéobotanique : sociétés, pratiques, environnements (AASPE) UMR 7209 Muséum national d’Histoire naturelle, CNRS, 55 rue Buffon, 75005 Paris cedex 05, France
Elisamara Sabadini-Santos
Affiliation:
Departamento de Geoquímica, Universidade Federal Fluminense, Outeiro São João Batista, s/n, Niterói, 24001-970, RJ, Brazil
Maria Dulce Gaspar
Affiliation:
Programa de Pós–Graduação em Arqueologia do Museu Nacional (PPGArq), Universidade Federal do Rio de Janeiro (UFRJ), Quinta da Boa Vista, s/n, Rio de Janeiro, 20940-40, RJ, Brazil
Kita Macario
Affiliation:
Laboratório de Radiocarbono, Instituto de Física, Universidade Federal Fluminense, Av. Gal. Milton Tavares de Souza s/n, 24210-346, Niterói, RJ, Brazil
Bruna da Silva Mota Neto
Affiliation:
Laboratório de Radiocarbono, Instituto de Física, Universidade Federal Fluminense, Av. Gal. Milton Tavares de Souza s/n, 24210-346, Niterói, RJ, Brazil
Olivier Tombret
Affiliation:
Archéozoologie, Archéobotanique : sociétés, pratiques, environnements (AASPE) UMR 7209 Muséum national d’Histoire naturelle, CNRS, 55 rue Buffon, 75005 Paris cedex 05, France
Denis Fiorillo
Affiliation:
Archéozoologie, Archéobotanique : sociétés, pratiques, environnements (AASPE) UMR 7209 Muséum national d’Histoire naturelle, CNRS, 55 rue Buffon, 75005 Paris cedex 05, France
Michel Lemoine
Affiliation:
Archéozoologie, Archéobotanique : sociétés, pratiques, environnements (AASPE) UMR 7209 Muséum national d’Histoire naturelle, CNRS, 55 rue Buffon, 75005 Paris cedex 05, France
Leandro Amaro Pessoa
Affiliation:
Departamento de pesquisa e engenharia, Instituto Virtual Internacional de Mudanças Globais (IVIG- COPPE / UFRJ), Universidade Federal do Rio de Janeiro (UFRJ), Cidade Universitária, Avenida Pedro Calmon s/n, 21941-596, RJ, Brazil
Sandrine Grouard
Affiliation:
Archéozoologie, Archéobotanique : sociétés, pratiques, environnements (AASPE) UMR 7209 Muséum national d’Histoire naturelle, CNRS, 55 rue Buffon, 75005 Paris cedex 05, France
Orangel Aguilera
Affiliation:
Departamento de Biologia Marinha, Universidade Federal Fluminense (UFF), Laboratório de Paleoecologia e Mudanças Globais (LP&MG). Campus Gragoatá, Bloco M, 24210-201, Niterói, RJ, Brazil
*
*Corresponding author. Email: Lopes_mariana@id.uff.br
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Abstract

Isotopic analysis of Micropogonias furnieri otoliths were used to get insight into palaeoceanographic conditions in the Guanabara Bay and Saquarema Lagoon, Rio de Janeiro state (RJ), located on the southeastern coast of Brazil, under upwelling influence of the Cabo Frio system. Archaeological otoliths come from two Holocene shellmounds (or sambaquis): Galeão and Beirada. For the first time, radiocarbon analysis using high accuracy techniques were performed at Galeão. Age range was determined to be between 5820 and 4980 cal BP, which extends the chronology of human settlement in the Guanabara Bay. Micro-samples of the otoliths were collected sequentially from the core to the edge, to provide continuous δ18O and δ13C isotopic profiles over the lifetime of the individual fish. Derived-δ18Ooto palaeotemperature estimates vary according to seasonality, resulting in a palaeoceanographic variation between 8 to 31°C for Guanabara Bay and 8 and 28°C for the Saquarema Lagoon. Our data indicate that whitemouth croakers were captured during the Middle Holocene from the Guanabara Bay and Saguarema Lagoon and resided in cooler temperatures compared to temperatures of current conditions.

Keywords

AtlanticHolocene water massesPalaeoceanographyPalaeothermometerupwellingwhitemouth croaker
Type
Research Article
Information
Radiocarbon , Volume 64 , Issue 5 , October 2022 , pp. 1109 - 1137
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Copyright
© The Author(s), 2022. Published by Cambridge University Press for the Arizona Board of Regents on behalf of the University of Arizona

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