Evidence for early Pliocene and late Miocene transgressions in southern Patagonia (Argentina): Sr-87/Sr-86 ages of the pectinid "Chlamys" actinodes (Sowerby)

• Main Authors: del Rio, CJ, Griffin, M, McArthur, JM, Martinez, S, Thirlwall, MF
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2013
• Subjects: Tortonian; Late Miocene; Zanclean; Early Pliocene; Patagonia; Argentina; Sr-87/Sr-86; Austral; Cockburn; Antarc*; Antarctica
• Online Access: https://discovery.ucl.ac.uk/id/eprint/1415940/1/1-s2.0-S0895981113001181-main.pdf; https://discovery.ucl.ac.uk/id/eprint/1415940/

Numerical ages based on 87Sr/86Sr dating of calcitic shells belonging to the pectinid “Chlamys” actinodes (Sowerby) document the only late Miocene (Tortonian) sea flooding event in the Austral Basin at Cabo Buentiempo (8.95 ± 0.82 Ma, 2 s.e.), and provide evidence of the first documented early Pliocene (Zanclean) transgression in Argentina recorded at Cañadón Darwin (5.15 ± 0.18 Ma, 2 s.e., Austral Basin) and at Terraces of Cerro Laciar (5.10 ± 0.21 Ma, 2 s.e.), southern San Jorge Basin). The sedimentary rocks deposited during the Tortonian are correlated with the youngest beds deposited by the “Entrerriense Sea” that covered northern Patagonia. The Zanclean marine episode is correlated with the long-term cycle represented in the Southern Hemisphere by the flooding events recorded in Cockburn and James Ross Islands (Antarctica) and in North-Central Chile.