PUMA
Istituto di Scienze Marine     
Marcano M., Mukasa S., Lohmann K., Stefano C., Andronikov A., Taviani M. Chronostratigraphic and paleoenvironmental constraints derived from the Sr-87/Sr-86 and delta O-18 signal of Miocene bivalves, Southern McMurdo Sound, Antarctica. In: Global and Planetary Change, vol. 69 (3) pp. 124 - 132. ELSEVIER SCIENCE BV, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS, 2009.
 
 
Abstract
(English)
87Sr/86Sr measurements were carried out on samples of various macrofossil taxa recovered from the SMS AND-2A core with the main goal of improving age control of the core, and provide insight on marine climate at the time of carbonate precipitation. Shell material was carefully screened using cathodoluminescence (CL) to discern optimum areas for microdrilling. Powders thus obtained were in addition analyzed for Ca, Mg, Sr, Mn, and Fe contents to further evaluate the possibility of diagenetic alteration of the skeletal carbonate before measuring their Sr isotope compositions. Bivalves turned out to be the best candidates for isotopic determinations. Unaltered calcitic bivalves produced reliable 87Sr/86Sr age ranges. Aragonitic material, on the other hand, produced less radiogenic 87Sr/86Sr than anticipated, an unexpected result. Preliminary oxygen isotope determinations in calcite samples confirm contrasting marine climate conditions between the late Early Miocene (16.516.0 Ma), and the early Late Miocene (~11 Ma).
DOI: 10.1016/j.gloplacha.2009.05.001
Subject McMurdo Sound
paleoclimatology
veneridae
aragonite
Sr-87/Sr-86
O-18/O-16


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