| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2002PPP...181...91J |
| P356 | DOI | 10.1016/S0031-0182(01)00474-6 |
| P50 | author | Christian Ostertag-Henning | Q63974863 |
| P2093 | author name string | K.H Freeman | |
| M.M Joachimski | |||
| R.D Pancost | |||
| W Buggisch | |||
| P2860 | cites work | Interpreting carbon-isotope excursions: Strangelove oceans | Q61660437 |
| 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 | ||
| Water column anoxia, enhanced productivity and concomitant changes in δ13C and δ34S across the Frasnian–Famennian boundary (Kowala — Holy Cross Mountains/Poland) | Q63972084 | ||
| Late Middle Ordovician environmental change and extinction: Harbinger of the Late Ordovician or continuation of Cambrian patterns? | Q67215567 | ||
| Interpreting carbon-isotope excursions: carbonates and organic matter | Q96965436 | ||
| Consistent fractionation of 13C in nature and in the laboratory: growth-rate effects in some haptophyte algae. | Q43530959 | ||
| Isotopic biogeochemistry of the Oxford Clay Formation (Jurassic), UK. | Q47241257 | ||
| 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 | ||
| The abundance of 13C in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 Ma | Q55967232 | ||
| GEOCARB II; a revised model of atmospheric CO 2 over Phanerozoic time | Q56001352 | ||
| New U–Pb zircon ages and the duration and division of Devonian time | Q56048502 | ||
| 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 | ||
| Constraints on the formation of sedimentary dolomite | Q57228426 | ||
| 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 | ||
| Geochemical and climatic effects of increased marine organic carbon burial at the Cenomanian/Turonian boundary | Q59071406 | ||
| Organic geochemical indicators of palaeoenvironmental conditions of sedimentation | Q59072111 | ||
| Frasnian/Famennian mass extinction and cold-water oceans | Q59609438 | ||
| Late Devonian “Kellwasser Event” mass-extinction horizon in Germany: No geochemical evidence for a large-body impact | Q59609507 | ||
| Effect of the Frasnian-Famennian extinction event on the stromatoporoids | Q59666167 | ||
| Geochemical evidence for a catastrophic biotic event at the Frasnian/Famennian boundary in south China | Q61660317 | ||
| P433 | issue | 1-3 | |
| P921 | main subject | geochemistry | Q161764 |
| paleoecology | Q1337995 | ||
| P304 | page(s) | 91-109 | |
| P577 | publication date | 2002-06-01 | |
| P1433 | published in | Palaeogeography, Palaeoclimatology, Palaeoecology | Q7126415 |
| P1476 | title | Carbon isotope geochemistry of the Frasnian–Famennian transition | |
| P478 | volume | 181 |
| Q98184175 | Anchoring the Late Devonian mass extinction in absolute time by integrating climatic controls and radio-isotopic dating |
| Q59841467 | Carbon isotopic evidence for the associations of decreasing atmospheric CO2level with the Frasnian-Famennian mass extinction |
| 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 |
| Q64013322 | Deciphering the roles of environment and development in the evolution of a Late Triassic assemblage of conodont elements |
| Q58206722 | Deep-water anoxia over the Frasnian-Famennian boundary (La Serre, France): a tectonically induced oceanic anoxic event? |
| Q58457680 | Depositional evolution of a lower Paleozoic portion of the Southalpine domain: the Mt. Pizzul area (Carnic Alps, Italy) |
| Q56094962 | Impacts, volcanism and mass extinction: random coincidence or cause and effect? |
| Q58070972 | Investigating Devonian trees as geo-engineers of past climates: linking palaeosols to palaeobotany and experimental geobiology |
| Q59781692 | Late Devonian carbon isotope stratigraphy and sea level fluctuations, Canning Basin, Western Australia |
| Q58206714 | Mountain building-enhanced continental weathering and organic carbon burial as major causes for climatic cooling at the Frasnian-Famennian boundary (c. 376 Ma)? |
| Q56553187 | Oxygenation as a driver of the Great Ordovician Biodiversification Event |
| Q55431026 | Precisely dating the Frasnian-Famennian boundary: implications for the cause of the Late Devonian mass extinction. |
| Q41694937 | Thresholds of catastrophe in the Earth system |
| Q48353686 | Timing and pacing of the Late Devonian mass extinction event regulated by eccentricity and obliquity |
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