Results 161 to 170 of about 36,407 (282)
A new genus of giant salamander (Urodela, Cryptobranchidae) from the Pliocene of Japan. [PDF]
Noda M, Matsui M, Nishikawa K.
europepmc +1 more source
Abstract The seismic behavior of subduction megathrusts varies spatially and is influenced by the properties of subducting plates, including their sedimentary cover. Characterizing these subduction inputs is essential for understanding the mechanisms behind fault slip variability.
Philip M. Barnes +12 more
wiley +1 more source
First of a line or last of a dynasty? Parabos tigneresi and the evolution of eurasian bovinae in the early pliocene. [PDF]
Sorbelli L +7 more
europepmc +1 more source
Abstract Volcanism in continental rifts, rifted volcanic arcs, and back‐arc basins is fundamentally coupled with crustal extension. However, the precise geometry and timing of the fault systems that facilitate magma transport and accommodate extension remain poorly constrained.
Jonas Preine +17 more
wiley +1 more source
Phylogenetic insights into the diversification of cutting strategies in leaf-cutting ants. [PDF]
Sánchez-Restrepo AF +2 more
europepmc +1 more source
Abstract Glacial‐interglacial cycles increased in length from about 41 to 100 thousand years during the Middle Pleistocene Transition (MPT) about 1.5 to 0.8 million years ago. This took place in step with strong global cooling after several million years of weaker cooling.
G. Shaffer +2 more
wiley +1 more source
The Opoiti, Whakapunake and Tahaenui Limestone formations (Opoitian to Waipipian; Pliocene) crop out extensively in northern Hawke’s Bay between Wairoa and Mahia Peninsula where they are encased within mudstone dominated Wairoa Formation.
Drinnan, Michele Maree
core
Out of the tropics and adaptation in the Asian subtropics of Dendrobium section Dendrobium (Orchidaceae). [PDF]
Zhou P +8 more
europepmc +1 more source
Arc Heat Flow and Magmatic Heat Budgets
Abstract We evaluate hydrothermal heat loss from 11 volcanic‐arc segments (∼6,000 km of arc length, ∼10% of the global total), motivated by the observation that much magmatic heat ultimately crosses the land surface as heated aqueous fluid. Heat loss takes place by volcanic eruption, geothermal heat conduction to the surface, fumarolic (vapor ...
S. E. Ingebritsen +7 more
wiley +1 more source
Repeated major inland retreat of Thwaites and Pine Island glaciers (West Antarctica) during the Pliocene. [PDF]
Horikawa K +13 more
europepmc +1 more source

