A basal dinosaur from the dawn of the dinosaur era in southwestern PangaeaEccentricity and obliquity paced carbon cycling in the Early Triassic and implications for post-extinction ecosystem recoveryCO2-forced climate and vegetation instability during Late Paleozoic deglaciation.Climate and vegetational regime shifts in the late Paleozoic ice age earthBiological skeletal carbonate records changes in major-ion chemistry of paleo-oceansDynamic Carboniferous tropical forests: new views of plant function and potential for physiological forcing of climate.Early Permian (Asselian) vegetation from a seasonally dry coast in western equatorial Pangea: Paleoecology and evolutionary significanceCO2 as a primary driver of Phanerozoic climateClimate, p CO 2 and terrestrial carbon cycle linkages during late Palaeozoic glacial–interglacial cyclesThe Late Paleozoic Ice Age: An Evolving ParadigmLate Pennsylvanian aridification on the southwestern margin of Gondwana (Paganzo Basin, NW Argentina): A regional expression of a global climate perturbationThe evolution of the global selenium cycle: Secular trends in Se isotopes and abundancesGeologic map and upper Paleozoic stratigraphy of the Marble Canyon area, Cottonwood Canyon quadrangle, Death Valley National Park, Inyo County, CaliforniaMillennial-scale variations in western Sierra Nevada precipitation during the last glacial cycle MIS 4/3 transitionStrontium and carbon isotopic evidence for decoupling of pCO2 from continental weathering at the apex of the late Paleozoic glaciationLate Paleozoic tropical climate response to Gondwanan deglaciationEccentricity-paced late Paleozoic climate changeBasin-Wide Diagenetic Patterns: Integrated petrologic, Geochemical and Hydrologic ConsiderationsMeteoric diagenesis and fluid-rock interaction in the Middle Permian Capitan backreef: Yates Formation, Slaughter Canyon, New MexicoEvolutionary differences in Δ13C detected between spore and seed bearing plants following exposure to a range of atmospheric O2:CO2 ratios; implications for paleoatmosphere reconstructionReply to comment on “Was atmospheric CO 2 capped at 1000 ppm over the past 300 million years?” [Palaeogeogr. Palaeoclimatol. Palaeoecol. 441 (2016) 653–658]Was atmospheric CO2 capped at 1000 ppm over the past 300 million years?Cyclic changes in Pennsylvanian paleoclimate and effects on floristic dynamics in tropical PangaeaEvolution of moisture transport to the western U.S. during the last deglaciationStalagmite records of hydroclimate in central California during termination 1Response of a modern cave system to large seasonal precipitation variabilityModeling speleothem δ13C variability in a central Sierra Nevada cave using 14C and 87Sr/86SrLate Pleistocene California droughts during deglaciation and Arctic warmingMineralogical and geochemical evolution of a basalt-hosted fossil soil (Late Triassic, Ischigualasto Formation, northwest Argentina): Potential for paleoenvironmental reconstruction40Ar/39Ar dating of Late Permian evaporites, southeastern New Mexico, USAToward an orbital chronology for the early Aptian Oceanic Anoxic Event (OAE1a, ~120 Ma)Evolution of Cupido and Coahuila carbonate platforms, Early Cretaceous, northeastern MexicoIntegrated Sr isotope variations and sea-level history of Middle to Upper Cambrian platform carbonates: Implications for the evolution of Cambrian seawater 87Sr/86SrDiagenetic evaluation of a Pennsylvanian carbonate succession (Bird Spring Formation, Arrow Canyon, Nevada, U.S.A.) — 1: Brachiopod and whole rock comparisonCarboniferous climate teleconnections archived in coupled bioapatite δ18OPO4 and 87Sr/86Sr records from the epicontinental Donets Basin, UkraineTesting the accuracy of new paleoatmospheric CO2 proxies based on plant stable carbon isotopic composition and stomatal traits in a range of simulated paleoatmospheric O2:CO2 ratiosDynamic Carboniferous climate change, Arrow Canyon, NevadaSedimentology as a Key to Understanding Earth and Life ProcessesOrigin of paleovalleys on the Rio Grande do Sul Shield (Brazil): Implications for the extent of late Paleozoic glaciation in west-central GondwanaMapping Fluid‐Filled Inclusions in Stalagmites Using Coupled X‐Ray and Neutron Computed Tomography: Potential as a Water Excess Proxy
P50
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schweizerisch-amerikanische Geologin und Paläoklimatologin
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nr98012657
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0000-0003-0492-3796
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1960-03-17T00:00:00Z
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lccn-nr98012657