Results 191 to 200 of about 45,124 (291)
Rare fossil insect (Zekuforma maculata sp. nov) from the Tibetan plateau unveils adaptive innovations and extinction mechanisms. [PDF]
Dai R +5 more
europepmc +1 more source
Abstract We analyze Interferometric Synthetic Aperture Radar (InSAR) and Global Navigation Satellite System (GNSS) data to characterize ground deformation and dike opening associated with the May 2021 Nyiragongo eruption. Despite documented eruptions in 1977 and 2002, Nyiragongo's magmatic system and its interaction with regional rifting remain poorly ...
D. Murekezi +9 more
wiley +1 more source
Mid-Miocene warmth pushed fossil coral calcification to physiological limits in high-latitude reefs. [PDF]
Reuter M +5 more
europepmc +1 more source
Stochastic Resonance Elucidates the Emergence and Periodicity Transition of Glacial Cycles
Abstract Glacial cycles emerged with a 41‐kyr period after the Pliocene and later intensified with a 100‐kyr period in the mid‐Pleistocene, which were attributed to Earth's orbital variations. However, no significant changes in the orbital forcing were found at the two transitions, and the forcing was too small to drive these cycles. Here, a stochastic
Tian Xu, Gabriel Katul, Shineng Hu
wiley +1 more source
Savanna ecosystems and mammalian adaptations in Mid-Miocene Northern China. [PDF]
Li C +7 more
europepmc +1 more source
Altered Ocean Temperature Gradients Are Key to Miocene South Asian Monsoon Evolution
Abstract Indian Ocean sea surface temperature (SST) gradients influence South Asian summer monsoon (SASM) strength. Middle Miocene proxy records show reversed Arabian Sea zonal gradients (warmer west than east) and reduced Indian Ocean meridional gradients compared to today—patterns coupled models cannot reproduce, hindering accurate SASM simulation ...
Xiaoqing Liu, Matthew Huber
wiley +1 more source
A thermochronological transect across the Trento platform: constraints for the evolution of the European Eastern Southern Alps. [PDF]
Klotz T +4 more
europepmc +1 more source

