Insights into the distribution of shallow-marine to estuarine early miocene oysters from southwestern patagonia: Sedimentologic and stable isotope constraints

The lower Miocene Estancia 25 de Mayo Formation consists of shallowmarine to estuarine deposits that bear numerous oyster shell beds distributed throughout the succession. Facies analysis reveals that oysters grew in the nearshore paleoenvironments of both the lower Quién Sabe and the upper Bandurri...

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Autor principal: Cuitiño, J.I
Otros Autores: Santos, R.V, Scasso, R.A
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Publicado: SEPM Society for Sedimentary Geology 2013
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100 1 |a Cuitiño, J.I. 
245 1 0 |a Insights into the distribution of shallow-marine to estuarine early miocene oysters from southwestern patagonia: Sedimentologic and stable isotope constraints 
260 |b SEPM Society for Sedimentary Geology  |c 2013 
270 1 0 |m Cuitiño, J.I.; Universidad de Buenos Aires, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Intendente Guiraldes 2160 (C1428EHA), Ciudad Autónoma de Buenos Aires, Argentina; email: joseignacio@gl.fcen.uba.ar 
506 |2 openaire  |e Política editorial 
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520 3 |a The lower Miocene Estancia 25 de Mayo Formation consists of shallowmarine to estuarine deposits that bear numerous oyster shell beds distributed throughout the succession. Facies analysis reveals that oysters grew in the nearshore paleoenvironments of both the lower Quién Sabe and the upper Bandurrias members. Two oyster species were identified: Crassostrea(?) hatcheri, distributed in the lower two thirds of the column, and Crassostrea orbignyi, distributed in the upper third of the column within the transition from marine to the fluvial deposits of the overlying Santa Cruz Formation. Petrographic, cathodoluminiscence, and carbon and oxygen stable isotope analyses of individual growth increments were performed on carbonate from all the oyster beds, together with consecutive time-series analyses for one specimen of each species. The isotopic composition of the shell seems to be associated with the microstructure of the growth increments. Selective diagenetic alteration affected chalky growth increments; whereas translucent (foliated and prismatic) growth increments are well preserved and can be used to infer paleoenvironmental conditions. Isotopic data indicate that C.(?) hatcheri lived in normal marine waters with a range of paleotemperatures from 10.6 to 20.5 °C. Monospecific beds of this oyster are related to opportunistic and quick colonization of the sea bottom. More negative δ13C and δ18O values in C. orbignyi shells likely reflect decreased paleosalinities, and the resultant environmental stress controlled the development of these low-diversity oyster accumulations. The separate stratigraphic distribution of each species was therefore determined by the paleoenvironmental conditions. © 2013, SEPM (Society for Sedimentary Geology).  |l eng 
593 |a Universidad de Buenos Aires, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Intendente Guiraldes 2160 (C1428EHA), Ciudad Autónoma de Buenos Aires, Argentina 
593 |a Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires, Intendente Guiraldes 2160 (C1428EHA), Ciudad Autónoma de Buenos Aires, Argentina 
593 |a Universidade de Brasília, Instituto de Geociencias, Campus Universitário, Darcy Ribeiro CEP 70910-900 Brasília, DF, Brazil 
650 1 7 |2 spines  |a CARBON 
690 1 0 |a CARBONATE 
690 1 0 |a COLONIZATION 
690 1 0 |a ENVIRONMENTAL STRESS 
690 1 0 |a FACIES ANALYSIS 
690 1 0 |a ISOTOPIC COMPOSITION 
690 1 0 |a MICROSTRUCTURE 
690 1 0 |a MOLLUSC 
690 1 0 |a OXYGEN 
690 1 0 |a SHELL 
690 1 0 |a STABLE ISOTOPE 
690 1 0 |a SUCCESSION 
690 1 0 |a BRAZIL 
690 1 0 |a ESTANCIA 
690 1 0 |a PATAGONIA 
690 1 0 |a SERGIPE 
700 1 |a Santos, R.V. 
700 1 |a Scasso, R.A. 
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