LITHOCHEMICAL AND FLORAL EVIDENCE FOR RECONSTRUCTION OF THE MESOZOIC PALEOCLIMATE, AS EXEMPLIFIED FROM THE BUREYA BASIN, FAR EAST OF RUSSIA [PDF]
С. А. Медведева
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Author Correction: Niche partitioning shaped herbivore macroevolution through the early Mesozoic [PDF]
Suresh A. Singh +5 more
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An overview of the postcranial osteology of caecilians (Gymnophiona, Lissamphibia)
Abstract Caecilians comprise a relatively small (~220 species) group (Gymnophiona) of snake‐like or worm‐like, mostly tropical amphibians. Most adult caecilians are fossorial, although some species may live in aquatic or semi‐aquatic environments, either as larvae or adults.
Rodolfo Otávio Santos +2 more
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Evolution of Insect Pollination Before Angiosperms and Lessons for Modern Ecosystems. [PDF]
Negri I, Toledo ME.
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Tabulation of uranium and thorium data on the Mesozoic-Cenozoic intrusive rocks of known chemical composition in Colorado [PDF]
George Phair, Lillie B. Jenkins
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Abstract This study investigates the occurrence of osteomyelitis in non‐avian dinosaurs, focusing on the Ibirá locality, a site with a high incidence of this pathological condition. We analyzed six new osteopathic sauropod specimens from the Upper Cretaceous of Brazil.
Tito Aureliano +3 more
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Morphology of male genitalia, legs, and wing venation reveals the classification of Mesozoic Zoraptera (Insecta). [PDF]
Kočárek P, Kočárková I, Kundrata R.
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Body Size Evolution in Burying Beetles (Staphylinidae: Silphinae: Nicrophorus)
Burying beetles (genus Nicrophorus) exhibit broad, skewed variation in body size, which influences carcass use and competitive interactions. Using a large dataset of morphological and geographic data, we show that body size evolution is shaped by phylogenetic history, biogeography, and ecological interactions, with divergence especially pronounced ...
Ashlee N. Smith +6 more
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The timing and nature of marine ecosystem recovery following the Permian-Triassic mass extinction. [PDF]
Nicholls AL +5 more
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Eighteen boreholes in Colombia's Tropical Andes reveal elevation‐controlled Critical Zone architecture. Four‐layer weathering profiles with thick saprolite (≤48 m) form at high elevations (>1,100 m) where dense fracturing enhances permeability. Low‐elevation boreholes lack saprolite despite high fracture density, demonstrating fracturing's dual role as
Helbert Garcia‐Delgado +2 more
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