Hardgrounds are important surfaces for basin analysis and oil exploration, representing in some cases significant markers of the sedimentary basin fill. In the Neuquén Basin, bioerosion structures are common on the shell surfaces of benthic organisms, but bioeroded hardgrounds are comparatively uncommon. In the Pilmatué Member of the Lower Cretaceous Agrio Formation (Valanginian-Hauterivian) two examples of bioeroded hardgrounds are described in detail, allowing to recognize contrasting palaeoenvironmental and sequence-stratigraphic contexts, and in turn, discussing the potential major controlling factors in each example. In both cases Trypanites isp. and Gastrochaenolites isp. are described, interpreted as belonging to a Trypanites ichnofa...
Macroids, cm-sized biogenically coated grains made of associations of metazoans or protozoans, accum...
The Lower Cretaceous Agrio Formation is a source rock considered to be a possible unconventional res...
In-depth ichnological studies of Lower Cretaceous, marginal-marine facies from the Agrio Formation (...
The Intra-Valanginian Discontinuity in the Neuquén Basin (Argentina) marks a dramatic sea-level fall...
Omission surfaces represent a gap in the sedimentary record on a particular environment, constitutin...
Large-scale depositional and paleogeographic reconstructions of shallow-marine to continental units ...
Forced-regressive conditions have been widely described by sequence-stratigraphic conceptual models,...
Shorefaces can display strong facies variability and integration of sedimentology and ichnology prov...
In the Lago San Martín region (Santa Cruz Province, Argentina), the Springhill Formation (50–100 m t...
The interpretation of sharp-based shallow-marine sandstone bodies encased in offshore mudstones, par...
Hard-substrate communities of the Early Cretaceous marine units of the Neuquén Basin (Argentina) wer...
Shorefaces can display strong facies variability and integration of sedimentology and ichnology prov...
Shallow-marine successions deposited during long-term transgressions are considered to develop relat...
Thick (10s of m) successions of highly bioturbated, storm-influenced shallow-marine deposits are rel...
During the Late Cretaceous, the Austral-Magallanes Basin (AMB) records the change from a thermal sub...
Macroids, cm-sized biogenically coated grains made of associations of metazoans or protozoans, accum...
The Lower Cretaceous Agrio Formation is a source rock considered to be a possible unconventional res...
In-depth ichnological studies of Lower Cretaceous, marginal-marine facies from the Agrio Formation (...
The Intra-Valanginian Discontinuity in the Neuquén Basin (Argentina) marks a dramatic sea-level fall...
Omission surfaces represent a gap in the sedimentary record on a particular environment, constitutin...
Large-scale depositional and paleogeographic reconstructions of shallow-marine to continental units ...
Forced-regressive conditions have been widely described by sequence-stratigraphic conceptual models,...
Shorefaces can display strong facies variability and integration of sedimentology and ichnology prov...
In the Lago San Martín region (Santa Cruz Province, Argentina), the Springhill Formation (50–100 m t...
The interpretation of sharp-based shallow-marine sandstone bodies encased in offshore mudstones, par...
Hard-substrate communities of the Early Cretaceous marine units of the Neuquén Basin (Argentina) wer...
Shorefaces can display strong facies variability and integration of sedimentology and ichnology prov...
Shallow-marine successions deposited during long-term transgressions are considered to develop relat...
Thick (10s of m) successions of highly bioturbated, storm-influenced shallow-marine deposits are rel...
During the Late Cretaceous, the Austral-Magallanes Basin (AMB) records the change from a thermal sub...
Macroids, cm-sized biogenically coated grains made of associations of metazoans or protozoans, accum...
The Lower Cretaceous Agrio Formation is a source rock considered to be a possible unconventional res...
In-depth ichnological studies of Lower Cretaceous, marginal-marine facies from the Agrio Formation (...