Results 111 to 120 of about 9,376 (253)
Abstract We present the first micrometer‐scale, phase‐resolved compositional characterization of impact melt glass from the Hapcheon crater (~1.4 km apparent diameter), the first confirmed impact structure on the Korean Peninsula, integrating EPMA‐WDS (5 μm spot), confocal Raman spectroscopy (<1 μm spot), XRD, and 40Ar/39Ar step‐heating geochronology ...
Jin‐Young Lee +2 more
wiley +1 more source
Protoma kayalensis Late Miocene
Protoma kayalensis (Dey, 1961)Fig. 2E–GTurritella kayalensis Dey, 1961: 59, pl. 7 fig. 18.Protoma kayalensis – Kulkarni et al. 2010: 315, fig. 2(h).Non Turritella harrisoni Cox, 1936: pl. 8 figs 27, 29 (misidentification).Material examinedIRAN – Sistan and Baluchestan • 10 shells; Dar Pahn Unit; GDZU-0011 to GDZU-0020.RemarksDey ...
Kiel, Steffen +3 more
openaire +1 more source
Evolution of spinescence in mimosoid legumes. Summary The evolutionary arms race between plants and herbivores led to numerous plant adaptations, including spinescence. However, the balance between herbivory and abiotic conditions in the evolution of spinescence remains unclear. We integrated phylogenetic, geographic, and trait data for 2686 species of
Rachel Souza Ferreira +6 more
wiley +1 more source
Savanna ecosystems and mammalian adaptations in Mid-Miocene Northern China
The paleoenvironments and ecosystems of northern China during the Miocene (ca. 23–5.3 Ma) are complex topics, especially concerning the uplift of the Tibetan Plateau on the surrounding areas and the ecological adaptations of mammals as a consequence. Our
Chunxiao Li +7 more
doaj +1 more source
CO2-forced Late Miocene cooling and ecosystem reorganizations in East Asia. [PDF]
Wen Y +7 more
europepmc +1 more source
ABSTRACT Microporous carbonate rocks typically record complex diagenetic histories driven by microbial activity and fluid interactions within multiple diagenetic environments. The relative roles of meteoric and burial diagenetic processes in pore evolution remain debated, particularly within Cretaceous carbonate systems of the Middle East, as does the ...
Hugues Bitault +5 more
wiley +1 more source
The Mura-Zala basin was formed due to ENE-WSW trending crustal extension in the late early and middle Miocene (19 – 11 Ma). Marine sedimentation occurred in several more or less confined depressions (half grabens), then in a unified basin.
Laszlo Fodor +8 more
doaj
Warm, not cold temperatures contributed to a Late Miocene reef decline in the Coral Sea. [PDF]
Petrick B +5 more
europepmc +1 more source
Cenozoic tropical carbonate platforms in the Santos Basin, SE Brazilian Margin
ABSTRACT Tropical carbonate platforms accompanied the latitudinal shifts of the tropical belt throughout the Cenozoic. Their flat‐topped geometries were influenced by a specific set of processes, including climate and sea‐level changes, carbonate facies, tectonics and continental runoff.
Mateus Gama +5 more
wiley +1 more source
ABSTRACT Significant porosity of more than 5% was found at depths of more than 8500 m in poorly sorted, calcareous mudstones of the Malmian Mikulov Formation. These overpressured rocks are the main hydrocarbon source rock in the Vienna Basin. Core samples from present‐day depths of 8150 m to 8550 m were analysed using X‐ray diffraction and scanning ...
Susanne Gier +3 more
wiley +1 more source

