Zobrazeno 1 - 10
of 16
pro vyhledávání: '"J. Andrew Beard"'
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-10 (2021)
Abstract The fossil record can illuminate factors that contribute to extinction risk during times of global environmental disturbance; for example, inferred thermal tolerance was an important predictor of extinction during several mass extinctions th
Externí odkaz:
https://doaj.org/article/9f80b547088b453c960f20527fb5f112
Publikováno v:
PALAIOS. 37:539-551
Skeletobionts, organisms that attach to or bore into the skeleton of a host, provide a useful system to observe biological interactions over geological timescales. We examined skeletobionts on brachiopod hosts from a stratigraphic section in western
Publikováno v:
Proceedings of the Royal Society B: Biological Sciences. 290
Studies of the fossil record can inform our understanding of not only the causes of mass extinctions, but also their effects on biodiversity, ecology and evolution. Here, we examine regional-scale ecological changes resulting from a Late Devonian mas
The fossil record can illuminate factors that contribute to extinction risk during times of global environmental disturbance; for example, inferred thermal tolerance is an important predictor of extinction during several mass extinctions that corresp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b60f68f6cd2bd4f8765166a7e23e7a64
https://doi.org/10.21203/rs.3.rs-622347/v1
https://doi.org/10.21203/rs.3.rs-622347/v1
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Andrew M. Bush, J. Andrew Beard, Sarah K. Brisson, James P. Kerr, Jaleigh Q. Pier, Anjali M. Fernandes
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Earth and Planetary Science Letters. 425:219-231
Oxygen isotope compositions of marine carbonates are commonly employed for understanding ancient temperatures, but this approach is complicated in the very distant past due to uncertainties about the effects of diagenesis and the isotopic composition
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 433:233-246
The Frasnian–Famennian boundary (Upper Devonian) is exposed in a 200 km-long outcrop belt in New York State, with deeper paleoenvironments to the west and shallower ones to the east. Geochronology in the eastern end of the outcrop belt has been bas