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Paul R. Renne

Researcher at Berkeley Geochronology Center

Publications -  374
Citations -  32299

Paul R. Renne is an academic researcher from Berkeley Geochronology Center. The author has contributed to research in topics: Basalt & Lava. The author has an hindex of 89, co-authored 363 publications receiving 29354 citations. Previous affiliations of Paul R. Renne include University of California, Berkeley & Planetary Science Institute.

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A Basal Dinosaur from the Dawn of the Dinosaur Era in Southwestern Pangaea

TL;DR: A previously unidentified basal theropod is described, its contemporary Eoraptor is reassessed as a basal sauropodomorph, the faunal record of the Ischigualasto Formation is divided with biozones, and the formation is bracketed with 40Ar/39Ar ages.
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Age of Etendeka flood volcanism and associated intrusions in southwestern Africa

TL;DR: In this paper, 40Ar/39Ar laser step-heating analyses of mineral separates from five volcanic units and five intrusions in Namibia yield important geochronological data for the Etendeka igneous province.
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State shift in Deccan volcanism at the Cretaceous-Paleogene boundary, possibly induced by impact.

TL;DR: High-precision dating of Deccan Traps volcanic units suggests an increase in volcanism associated with the Chicxulub impact, which suggests postextinction recovery of marine ecosystems was probably suppressed until after the accelerated volcanism waned.
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Ecological and temporal placement of early Pliocene hominids at Aramis, Ethiopia

TL;DR: Radioisotopic dating, geochem-ical analysis of interbedded volcanic ashes and biochronological considerations place the hominid-bearing deposits in the Middle Awash research area of Ethiopia's Afar depression at around 4.4 million years of age.
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Early and Late Alkali Igneous Pulses and a High-3He Plume Origin for the Deccan Flood Basalts

TL;DR: Rocks from the older complexes show a 3He/4He ratio of 14.0 times the air ratio, an initial 87Sr/86Sr ratio of 0.70483, and other geochemical characteristics similar to ocean island basalts; the later alkalic pulse shows isotopic evidence of crustal contamination.