Exposed mollusc shells may act as benthic islands in soft bottoms, and the analysis of their encrusting faunas provides unique palaeoecological information. In the late Valanginian of the Agrio Formation (Neuquén Basin, west-central Argentina), the large pectinid Prohinnites acted as a benthic island on soft substrates. Inequivalved Prohinnites adults with small, smooth cementing scars on the right valve suggest that a free reclining life habit followed the epibyssate juvenile and cementing phases. The encrusting fauna on Prohinnites was studied taxonomically and palaeoecologically by means of a quantitative approach. Over 90% of 123 valves presented encrusters. Encrustation was equally common in both valves. Internal encrustation was rare....
Trigoniide clams were conspicuous components of bivalve faunas in shallow seas during most of the Me...
Ostrea puelchana d?Orbigny, 1842 is a common species of commercial interest in Patagonia and is dist...
The Lower Cretaceous Chachao Formation in the Malargüe anticline area consists of wackestone, packst...
Trigonioid bivalves of the genus Steinmanella Crickmay are abundant at the top of the Vaca Muerta Fo...
Despite many advances in the study of the paleoecology of nautiloids and amonoids, there is still mu...
Hard-substrate communities of the Early Cretaceous marine units of the Neuquén Basin (Argentina) wer...
Lower Cretaceous (lower Hauterivian) oyster mass occurrences (OMOs) dominated by the gryphaeid small...
Sclerobiont communities have proven their environmental and taphonomic value in extant and past sett...
Shell morphology affects multiple aspects of the biology of ectocochleate cephalopods (e.g., floatab...
The Cretaceous Huitrín Formation in west-central Argentina records the final connection of the Neuq...
Shell concentrations are useful indicators of relative sea-level changes, systems tracts, and deposi...
This paper provides an updated taxonomic inventory of the bivalve fauna collected in the Pilmatué Me...
Late Quaternary marine skeletal concentrations from Argentina are rich in molluscs exhibiting a grea...
This work describes the composition and distribution of sclerobionts on the Miocene Patagonian oyste...
Field and laboratory observations of individual shells of 40 dominant taxa (19 gastropods, 21 bivalv...
Trigoniide clams were conspicuous components of bivalve faunas in shallow seas during most of the Me...
Ostrea puelchana d?Orbigny, 1842 is a common species of commercial interest in Patagonia and is dist...
The Lower Cretaceous Chachao Formation in the Malargüe anticline area consists of wackestone, packst...
Trigonioid bivalves of the genus Steinmanella Crickmay are abundant at the top of the Vaca Muerta Fo...
Despite many advances in the study of the paleoecology of nautiloids and amonoids, there is still mu...
Hard-substrate communities of the Early Cretaceous marine units of the Neuquén Basin (Argentina) wer...
Lower Cretaceous (lower Hauterivian) oyster mass occurrences (OMOs) dominated by the gryphaeid small...
Sclerobiont communities have proven their environmental and taphonomic value in extant and past sett...
Shell morphology affects multiple aspects of the biology of ectocochleate cephalopods (e.g., floatab...
The Cretaceous Huitrín Formation in west-central Argentina records the final connection of the Neuq...
Shell concentrations are useful indicators of relative sea-level changes, systems tracts, and deposi...
This paper provides an updated taxonomic inventory of the bivalve fauna collected in the Pilmatué Me...
Late Quaternary marine skeletal concentrations from Argentina are rich in molluscs exhibiting a grea...
This work describes the composition and distribution of sclerobionts on the Miocene Patagonian oyste...
Field and laboratory observations of individual shells of 40 dominant taxa (19 gastropods, 21 bivalv...
Trigoniide clams were conspicuous components of bivalve faunas in shallow seas during most of the Me...
Ostrea puelchana d?Orbigny, 1842 is a common species of commercial interest in Patagonia and is dist...
The Lower Cretaceous Chachao Formation in the Malargüe anticline area consists of wackestone, packst...