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Phytosaurs dominated freshwater aquatic environments during the Late Triassic era (235 to 201 million years ago) in North America, and are one of the more common vertebrate fossils that we find in the Chinle Formation.
Other hypotheses suggest that the warming and drying of the terrestrial environments during the Permian Period reduced the amount of organic matter buried in sediments as coal or petroleum, shifting the amount of organically fixed carbon dioxide that was recycled through the atmosphere.
It is a fluvial deposits formed under continental sedimentary environments during the Lower Cretaceous period.
The faunal assemblage indicates heterogeneous but relatively stable environments during the late Pleistocene.
However, robot may be faced with a variety of complex and changeable environments during the process of localization.
Mortality was low (1%) across both capture techniques and holding environments during the 14-day retention period.
Our findings suggest a complex interplay between oceanic basin and back-arc extension environments during the Santa Elena Ophiolite formation.
The sediments were deposited rapidly in glaciomarine, marine and submarine ice-contact environments during the Allerød and Younger Dryas periods.
Deposits of aeolian sand are known to have accumulated in periglacial environments during the cold phases of the late Quaternary.
The obtained data on variations in petromagnetic parameters, concentration of biogenic silica, and sediment compaction indicate considerable variations of sedimentary environments during the Late Pleistocene and Holocene.
Our combined approach shows no evidence for dense forested environments during the Early and Middle Turolian, and then supports previous hypotheses based on faunal analyses.
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