Glacial dysoxia in the deep subpolar North Atlantic during the Mid-Pleistocene Transition. [PDF]
Hernández-Almeida I +4 more
europepmc +1 more source
The 1931 Hawke's Bay earthquake (∼MS 7.8) stands as one of New Zealand's most devastating, causing widespread liquefaction and damage across the city of Napier. However, Napier remains underrepresented in liquefaction hazard studies as compared to other regions in the country.
Aavash Ghimire +3 more
wiley +1 more source
Major body size change in an extinct tropical island mammal associated with glacial-interglacial environmental shifts. [PDF]
Turvey ST +5 more
europepmc +1 more source
Retaining Models of Human Evolution After Repeated Falsifications—Why?
Two 19th century paradigms of human evolution emerged: Humans are subdivided into isolated populations in an evolutionary tree, versus human populations interbreed (gene flow) with no isolates. The tree model has been rejected whenever tested since the 1970's, whereas gene flow consistently fits.
Alan R. Templeton
wiley +1 more source
Plio-Pleistocene large carnivores from the Italian peninsula: functional morphology and macroecology
Meloro, Carlo
core
Eemian palaeogenetics demonstrates loss of diversity in modern fallow deer (<i>Dama dama</i>). [PDF]
Rocha-Méndez A +6 more
europepmc +1 more source
Phylogeographical studies of Amazonian birds have revealed large intraspecific diversity, even within recognized areas of endemism. To understand the origin and organization of Amazonian diversity, including the influence of current and historical landscapes, we need to evaluate fine‐scale patterns of genetic diversity in relation to detailed ...
Affonso Henrique Nascimento de Souza +4 more
wiley +1 more source
Earliest evidence of elephant butchery at Olduvai Gorge (Tanzania) reveals the evolutionary impact of early human megafaunal exploitation. [PDF]
Dominguez-Rodrigo M +11 more
europepmc +1 more source
Photosynthetic primary production in the Mesoproterozoic
Summary The Mesoproterozoic atmosphere had more CO2 and less O2 than at present. While the upper ocean was oxygenated, the deeper ocean was euxinic or ferruginous. Primary production was performed by Chlorobia, Cyanobacteria, Proteobacteria, and Archaeplastida.
Patricia Sánchez‐Baracaldo +1 more
wiley +1 more source
Late Cenozoic exhumation in the eastern Junggar Basin: Evidence from zircon (U-Th)/He ages of combustion metamorphic rocks. [PDF]
Chen B +6 more
europepmc +1 more source

