scholarly article | Q13442814 |
P819 | ADS bibcode | 2001ChGeo.175..109J |
P356 | DOI | 10.1016/S0009-2541(00)00365-X |
P50 | author | Jaap Sinninghe Damsté | Q15876790 |
Katherine H. Freeman | Q18686205 | ||
Richard D. Pancost | Q54552675 | ||
Grzegorz Racki | Q56577167 | ||
Christian Ostertag-Henning | Q63974863 | ||
Michael M Joachimski | Q64782282 | ||
P2093 | author name string | Harald Strauss | |
Ralf Littke | |||
P2860 | cites work | Extraterrestrial cause for the cretaceous-tertiary extinction | Q28244869 |
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Mechanisms of CO2 fixation in bacterial photosynthesis studied by the carbon isotope fractionation technique | Q41234598 | ||
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Impact winter and the Cretaceous/Tertiary extinctions: results of a Chicxulub asteroid impact model | Q47241263 | ||
A 6,000-year sedimentary molecular record of chemocline excursions in the Black Sea. | Q47263049 | ||
Fractionation of carbon isotopes by phytoplankton and estimates of ancient CO2 levels. | Q47290077 | ||
Evidence from carbon isotope measurements for diverse origins of sedimentary hydrocarbons | Q47346317 | ||
The post-Paleozoic chronology and mechanism of 13C depletion in primary marine organic matter. | Q47365235 | ||
An isotopic study of biogeochemical relationships between carbonates and organic carbon in the Greenhorn Formation | Q47369448 | ||
Iridium anomaly in the upper devonian of the canning basin, Western australia | Q47435777 | ||
Search for impact remains at the Frasnian-Famennian boundary in the stratotype area, southern France. | Q47782032 | ||
GEOCARB II; a revised model of atmospheric CO 2 over Phanerozoic time | Q56001352 | ||
A reappraisal of kerogen formation | Q56144909 | ||
Microbiological Fractionation of Sulphur Isotopes | Q56608838 | ||
Dependence of phytoplankton carbon isotopic composition on growth rate and [CO2)aq: Theoretical considerations and experimental results | Q56621104 | ||
Effect of Phytoplankton Cell Geometry on Carbon Isotopic Fractionation | Q56621108 | ||
A Thiosulfate Shunt in the Sulfur Cycle of Marine Sediments | Q56873999 | ||
The production of 34S-depleted sulfide during bacterial disproportionation of elemental sulfur | Q56874000 | ||
The use of chromium reduction in the analysis of reduced inorganic sulfur in sediments and shales | Q57179625 | ||
Molecular indicators of redox and marine photoautotroph composition in the late Middle Ordovician of Iowa, U.S.A | Q58098269 | ||
Restricted utility of the pristane/phytane ratio as a palaeoenvironmental indicator | Q59066083 | ||
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Tocopherols as likely precursors of pristane in ancient sediments and crude oils | Q59072207 | ||
A large and abrupt fall in atmospheric CO2 concentration during Cretaceous times | Q59095277 | ||
Geochemistry of recent TOC-rich sediments from the Gulf of California and the Black Sea | Q59309077 | ||
Ocean stagnation and ventilation defined by δ34S secular trends in pyrite and barite, Selwyn Basin, Yukon | Q59569860 | ||
Sulfur-isotope anomaly associated with the Frasnian-Famennian extinction, Medicine Lake, Alberta, Canada | Q59666505 | ||
Geochemical evidence for a catastrophic biotic event at the Frasnian/Famennian boundary in south China | Q61660317 | ||
Anoxic events in the late Frasnian—Causes of the Frasnian-Famennian faunal crisis? | Q61662099 | ||
Carbon and sulfur isotope anomalies across the Frasnian-Famennian extinction boundary, Alberta, Canada | Q63185403 | ||
2,3,6-/3,4,5-Trimethyl substituted diaryl carotenoid derivatives (Chlorobiaceae) in petroleums of the Belarussian Pripyat River Basin | Q63972111 | ||
Biosynthetic effects on the stable carbon isotopic compositions of algal lipids: implications for deciphering the carbon isotopic biomarker record | Q63972123 | ||
Diagenetic and catagenetic products of isorenieratene: Molecular indicators for photic zone anoxia | Q63972175 | ||
The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation | Q66731585 | ||
Late Middle Ordovician environmental change and extinction: Harbinger of the Late Ordovician or continuation of Cambrian patterns? | Q67215567 | ||
Carbon isotopic fractionation associated with lipid biosynthesis by a cyanobacterium: relevance for interpretation of biomarker records | Q74472046 | ||
Microtektites and mass extinctions: evidence for a late devonian asteroid impact | Q81210634 | ||
The influence of air and sea exchange on the carbon isotope distribution in the sea | Q107047002 | ||
P433 | issue | 1-2 | |
P921 | main subject | Poland | Q36 |
δ13C | Q3278929 | ||
δ34S | Q25325416 | ||
P304 | page(s) | 109-131 | |
P577 | publication date | 2001-05-01 | |
P1433 | published in | Chemical Geology | Q15756438 |
P1476 | title | Water column anoxia, enhanced productivity and concomitant changes in δ13C and δ34S across the Frasnian–Famennian boundary (Kowala — Holy Cross Mountains/Poland) | |
P478 | volume | 175 |
Q57320031 | A tale of shales: the relative roles of production, decomposition, and dilution in the accumulation of organic-rich strata, Middle–Upper Devonian, Appalachian basin |
Q58098223 | Carbon isotope geochemistry of the Frasnian–Famennian transition |
Q63044245 | Chapter 2Toward understanding Late Devonian global events: few answers, many questions |
Q58432003 | Chapter 8Productivity and bottom water redox conditions at the Frasnian-Famennian boundary on both sides of the Eovariscan Belt: constraints from trace-element geochemistry |
Q26749440 | Eutrophication, microbial-sulfate reduction and mass extinctions |
Q59781692 | Late Devonian carbon isotope stratigraphy and sea level fluctuations, Canning Basin, Western Australia |
Q55431026 | Precisely dating the Frasnian-Famennian boundary: implications for the cause of the Late Devonian mass extinction. |
Q57179566 | Production of15N-depleted biomass during cyanobacterial N2-fixation at high Fe concentrations |
Q58432019 | The Frasnian/Famennian boundary interval in the South Polish–Moravian shelf basins: integrated event-stratigraphical approach |
Q48353686 | Timing and pacing of the Late Devonian mass extinction event regulated by eccentricity and obliquity |
Q57235546 | Variations in Ce anomalies of conodonts through the Frasnian/Famennian boundary of Poland (Kowala – Holy Cross Mountains): implications for the redox state of seawater and biodiversity |
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