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Rio de Gallo
Paleoenvironments, taphonomy, and stable isotopic content of the terrestrial, fossil-vertebrate–bearing sequence of the El Disecado Member, El Gallo Formation, Upper Cretaceous, Baja California, México
Palaeomagnetism of Permo-Triassic rocks in the Iberian Cordillera, Spain: acquisition of Secondary and characteristic remanence
Potential Earliest Record of Podocnemidoid Turtles from the Early Cretaceous (Valanginian) of Colombia
Petroleum Developments in Mexico in 1969
Cretaceous Formations of Central America and Mexico
Strike-slip fault styles in slow-slipping oceanic transform faults—evidence from GLORIA surveys of Atlantis and Romanche Fracture Zones
Jurassic Formations of Gulf Region
A palynological investigation of funerary urn contents from the Roman Imperial age necropolis in Sardinia, Italy
Pollen rain, vegetation and connectivity in the Tacaná volcano, Southern Mexico
Structure and composition of the ocean–continent transition at an obliquely divergent transform margin, Gulf of Guinea, West Africa
Late Triassic stratigraphy and facies from northeastern Mexico: Tectonic setting and provenance
EMIL BÖSE’S SEARCH FOR AN ANCIENT LANDMASS
Geologic History of Northern Mexico and Its Bearing on Petroleum Exploration
NEOICHNOLOGY OF ARMADILLOS: KEYS FOR THE PALEOECOLOGICAL AND BEHAVIORAL INTERPRETATION OF FOSSIL TETRAPOD BURROWS
Abstract Tectonostratigraphic data derived from ongoing biostratigraphic, chronostratigraphic, paleobathymetric, paleobiogeographic, and lithostratigraphic investigations in west-central and east-central Mexico suggest that the Gulf of Mexico formed in two phases: Phase 1: Rifting and subsequent sea-floor spreading during the Late Jurassic (middle Oxfordian). All but the southwestern portion of the Gulf of Mexico formed during Phase 1. Phase 2: Northwest-to-southeast tectonic transport of allochthonous San Pedro del Gallo terrane remnants along the west side of Walper Megashear during the Middle Jurassic to Early Cretaceous. Where the stratigraphic successions are complete, megafossil data indicates that the San Pedro del Gallo terrane was situated at Southern Boreal paleolatitudes (>30° N) in the Nevadan back arc domain during the Middle Jurassic (late Bathonian to early Callovian) and was subsequently carried to lower paleolatitudes during the Late Jurassic and Early Cretaceous. For example, in the Huayacocotla remnant, the Boreal ammonite Kepplerites was recovered in the subsurface from the Palo Blanco Formation by Cantú-Chapa. In North America, Kepplerites is known from the Izee terrane (east-central Oregon), Western Interior (Montana and Saskatchewan), and northward to southern Alaska. Radiolarian, calpionellid, ammonite, and bivalve faunal data indicate that the Huayacocotla remnant had been transported to Northern Tethyan paleolatitudes (23° N to 29° N) during the Kimmeridgian and Tithonian and to Central Tethyan paleolatitudes (<23° N) by the beginning of the Early Cretaceous.
Basin Development and Tectonic History of the Llanos Basin, Eastern Cordillera, and Middle Magdalena Valley, Colombia
Late Cretaceous (Maastrichtian) ray-finned fishes from the island of Gavdos, southern Greece, with comments on the evolutionary history of the aulopiform teleost Enchodus
The Tropidoleptus carinatus controversy: Did this brachiopod occur in the Devonian of the Paraná Basin, Brazil?
Late Permian to Early Triassic transition in central and NE Spain: biotic and sedimentary characteristics
Abstract The Late Permian to Early Triassic (P/T) transition represents one of the most important Phanerozoic mass extinction episodes. Data from this transitional period are very scarce in continental basins, and reliable correlation with marine series is still a matter of debate. In this paper, information on the P/T transition in the continental series of central and NE Spain and the Balearic Islands is presented and compared with some coeval western European basins. The Iberian Ranges sections contain detailed information on the P/T transition, with sediments interpreted as alluvial fans, sandy and gravelly braided rivers and high sinuosity rivers with extensive floodplains, dated by means of pollen and spore assemblages. However, the fossil record contains two barren intervals throughout the study area, one in the Late Permian (Thuringian) and another during the latest Permian to Early Triassic. The possible causes of these gaps include the very likely relationship with the emplacement of the basaltic large igneous provinces (LIP) of SE China and western Siberia during this period of time.