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An independent evaluation of the Younger Dryas extraterrestrial impact hypothesisAbsence of geochemical evidence for an impact event at the Bølling-Allerød/Younger Dryas transitionIncomplete Bayesian model rejects contradictory radiocarbon data for being contradictoryThe Chicxulub asteroid impact and mass extinction at the Cretaceous-Paleogene boundaryReduced plumage and flight ability of a new Jurassic paravian theropod from ChinaSeasonal Cyclicity in Trace Elements and Stable Isotopes of Modern Horse EnamelComet or asteroid shower in the late Eocene?The formation of peak rings in large impact cratersReply to Bunch et al.: Younger Dryas impact proponents challenge new platinum group elements and osmium data unsupportive of their hypothesis.Microbial dissolution of hematite and associated cellular fossilization by reduced iron phases: a study of ancient microbe-mineral surface interactions.Solar system: lethal billiards.Timing and pacing of the Late Devonian mass extinction event regulated by eccentricity and obliquity.PLANET TOPERS: Planets, Tracing the Transfer, Origin, Preservation, and Evolution of their ReservoirS.End-Permian catastrophe by bolide impact: Evidence of a gigantic release of sulfur from the mantle: Comment and Reply: COMMENTArguments and Evidence Against a Younger Dryas Impact EventThe astronomical rhythm of Late-Devonian climate change (Kowala section, Holy Cross Mountains, Poland)Shelf hypoxia in response to global warming after the Cretaceous-Paleogene boundary impactRapid recovery of life at ground zero of the end-Cretaceous mass extinctionPresence of an iron-rich nanophase material in the upper layer of the Cretaceous-Tertiary boundary clayComment on the paper “Chicxulub impact predates K–T boundary: New evidence from Brazos, Texas” by Keller et al. (2007)Late Heavy BombardmentStrontium isotope analysis on cremated human remains from Stonehenge support links with west WalesQuantitative WD-XRF calibration for small ceramic samples and their source materialA 500-year seasonally resolved δ<sup>18</sup>O and δ<sup>13</sup>C, layer thickness and calcite aspect record from a speleothem deposited in the Han-sur-Lesse cave, BelgiumOrbital control on the timing of oceanic anoxia in the Late CretaceousPaleoclimate in continental northwestern Europe during the Eemian and early Weichselian (125–97 ka): insights from a Belgian speleothemReconstruction of MIS 5 climate in the central Levant using a stalagmite from Kanaan Cave, LebanonMercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction: COMMENTA transient deep-sea circulation switch during Eocene Thermal Maximum 2Chicxulub and the Exploration of Large Peak-Ring Impact Craters through Scientific DrillingEarth rocked by combination punchCorrigendum to “The impact of astronomical forcing on the Late Devonian greenhouse climate” [J. Glob. Planet. Chang. 120 C 2014 65–80]The impact of astronomical forcing on the Late Devonian greenhouse climateEvaluation of pneumatic nebulization and ns-laser ablation ICP-MS for bulk elemental analysis and 2-dimensional element mapping of iron meteoritesApplication of laser ablation-ICP-mass spectrometry for 2-dimensional mapping of element distributions in a Late Archean impact spherule layerNi-rich spinels and platinum group element nuggets condensed from a Late Archaean impact vapour cloudPetrology of impactites from El’gygytgyn crater: Breccias in ICDP-drill core 1C, glassy impact melt rocks and spherulesREE and Hf distribution among mineral phases in the CV–CK clan: A way to explain present-day Hf isotopic variations in chondritesTesting the ureilite projectile hypothesis for the El'gygytgyn impact: Determination of siderophile element abundances and Os isotope ratios in ICDP drill core samples and melt rocksAn emplacement mechanism for the mega-block zone within the Chicxulub crater, (Yucatán, Mexico) based on chemostratigraphy
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P50
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Philippe Claeys
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Philippe Claeys
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P106
P214
P1053
B-4895-2008
P1153
23079535700
P21
P214
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P3191
P3829
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0000-0002-4585-7687
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2000-01-01T00:00:00Z
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lccn-n2003016507