Fourteen pectinid and oyster species from the Pliocene Loreto Basin (Baja California Sur, Mexico) are recorded and discussed with regard to their relationships with closely related taxa. The whole assemblage points toward a Pliocene age. Aequipecten dallasi and Argopecten abietis abietis resulted to be the most useful biostratigraphic taxa, being restricted to Pliocene. The bulk of the considered species were confined within southern regions during the Pliocene. Crassostrea californica osunai is likely to have been endemic of Baja California Sur. Pectinids and oysters appear to have inhabited fine to coarse shallow infralittoral bottoms wave- or current-nfluenced. The environmental energy was the main factor controlling presence/absence of ...
Studies carried on in the last several years allow us to date the Canoa Formation as Late Pliocene. ...
A new pectinid, Lyropecten terrysmithae n. sp., has been recognized in middle to late Miocene rock u...
Microfossils including benthic and planktic foraminifera, ostracodes, calcareous algae, fish skeleta...
Fourteen pectinid and oyster species from the Pliocene Loreto Basin (Baja California Sur, Mexico) ar...
The present paper examines the molluscan and/or echinoid assemblages recovered from two lithostratig...
What is the applicability of present day biofacies and faunal assemblages for paleoenvironmental int...
This study focuses on reconstructing the dynamics within the Pliocene San Joaquin Basin (SJB) mollus...
We culled abundance record data from the NSF-funded TCN, Eastern Pacific Invertebrate Communities of...
AbstractThe Santa María Amajac paleolake is located in the central portion of Hidalgo, Mexico. Twent...
Taphonomy is a useful tool for enhancing paleoenvironmental interpretation. Holocene molluscan shell...
Terrestrial and marine palynomorph assemblages from a total of 42 productive samples from San Gregor...
A richly fossiliferous Pleistocene terrace located near Punta Chueca, Sonora, Mexico, contains sedim...
Typescript (photocopy).Evidence of organism interactions (predatory and non-predatory) in recent sam...
A palaeoecological study of sclerozoan foraminifera of the families Saccamminidae (aff. Sagenina), L...
Exposed mollusc shells may act as benthic islands in soft bottoms, and the analysis of their encrust...
Studies carried on in the last several years allow us to date the Canoa Formation as Late Pliocene. ...
A new pectinid, Lyropecten terrysmithae n. sp., has been recognized in middle to late Miocene rock u...
Microfossils including benthic and planktic foraminifera, ostracodes, calcareous algae, fish skeleta...
Fourteen pectinid and oyster species from the Pliocene Loreto Basin (Baja California Sur, Mexico) ar...
The present paper examines the molluscan and/or echinoid assemblages recovered from two lithostratig...
What is the applicability of present day biofacies and faunal assemblages for paleoenvironmental int...
This study focuses on reconstructing the dynamics within the Pliocene San Joaquin Basin (SJB) mollus...
We culled abundance record data from the NSF-funded TCN, Eastern Pacific Invertebrate Communities of...
AbstractThe Santa María Amajac paleolake is located in the central portion of Hidalgo, Mexico. Twent...
Taphonomy is a useful tool for enhancing paleoenvironmental interpretation. Holocene molluscan shell...
Terrestrial and marine palynomorph assemblages from a total of 42 productive samples from San Gregor...
A richly fossiliferous Pleistocene terrace located near Punta Chueca, Sonora, Mexico, contains sedim...
Typescript (photocopy).Evidence of organism interactions (predatory and non-predatory) in recent sam...
A palaeoecological study of sclerozoan foraminifera of the families Saccamminidae (aff. Sagenina), L...
Exposed mollusc shells may act as benthic islands in soft bottoms, and the analysis of their encrust...
Studies carried on in the last several years allow us to date the Canoa Formation as Late Pliocene. ...
A new pectinid, Lyropecten terrysmithae n. sp., has been recognized in middle to late Miocene rock u...
Microfossils including benthic and planktic foraminifera, ostracodes, calcareous algae, fish skeleta...