Sebastián Richiano

ICNOLOGÍA DE LA FORMACIÓN RÍO MAYER, CRETÁCICO INFERIOR, SUDOESTE DE GONDWANA, PATAGONIA, ARGENTINA

Abstract ICHNOLOGY OF THE RÍO MAYER FORMATION, LOWER CRETACEOUS, SOUTHWESTERN GONDWANA, PATAGONIA, ARGENTINA. The Río Mayer Formation was deposited during the Early Cretaceous in the Austral Basin (Santa Cruz Province, Argentina) and includes black shales with intercalated sandstones and marls. Abundant information is available on its palaeontological content, especially on ammonoids, but detailed ichnological studies are lacking. Sedimentological and ichnological data were collected in the Río Guanaco area (49°57′11″S—72°04′56″W). Three sections were identified and described in detail. The lower Section was deposited during the Berriasian—Valanginian and is composed of black shales. The middle section including black marls with intercalated black shales was deposited during the Valanginian—Hauterivian. The upper section is composed of black shales with frequent thin intercalations of finegrained sandstones (Barremian—Albian). Six ichnogenera were identified: Zoophycos, Chondrites, Bergaueria, Ophiomorpha, Palaeophycus and Teredolites. The most abundant and constant is Zoophycos, arranged in three morphological groups. All these ichnogenera are grouped —in the Río Mayer Formation— into two ichnoassociations. The first is found in the middle section, and is a typical Zoophycos ichnofacies with associated Bergaueria. The second ichnoassociation appears at the top of the upper section, and contains a Zoophycos ichnofacies with associated Ophiomorpha and Teredolites. The unusual presence of Bergaueria in low oxygen offshore environments, exceeds the bathymetric range typical of this ichnogenus. The unusual presence of O. cf. rudis in outer shelf environments reveals the existence of doomed pioneers in the analyzed unit.

Reading shell shape: implications for palaeoenvironmental reconstructions. A case study for bivalves from the marine Quaternary of Argentina (south-western Atlantic)

Most research on bivalves from the south-western Atlantic used morphological (shell) characters for taxonomic discriminations. Dominant Veneroids from Argentinian Quaternary coastal deposits exhibit wide morphological variation – often making objective discriminations difficult/impossible, which could be objectively described and compared through geometric morphometrics techniques. This work focuses on comparison of geometric morphometrics methods applied to fossil and modern shells, to assess inter- and intra-generic variations. Three approaches were considered: landmarks (L), semi-landmarks (SL) and outlines. Shell shape analyses for different time spans (Pleistocene, fossil Holocene and modern) and areas (Patagonia and Bonaerensian) showed that Elliptic Fourier analysis (EFA), Landmarks and Landmarks plus Semilandmarks (L+SL) can discriminate at generic levels: Mactra, Mulinia (Mactridae) vs. Pitar, Protothaca, Eurhomalea, Clausinella (Veneridae). L and L+SL are powerful for inter/intraspecific distinctions of Mactra. Variability of Mactra isabelleana includes the remaining nominal ‘species’ (transitional morphs). Causal environmental factors of (phenotype) variation could be addressed for modern environments (substrate, salinity and energy). Subtrigonal-inflated shells predominate in muddy, quieter, shallow mixo-polyhaline waters; ovate-elongate-compressed in sandy, poly-euhaline, deeper habitats. Differential spatial distribution (and abundance) across time responds to Late Quaternary high sea-level stands: transgressive maxima allowed higher salinity in marginal-marine areas and optimal conditions for Mactra isabelleana contrasting with scarcer records in the Mar Argentino today.