(Q63971964)

English

Synchronous negative carbon isotope shifts in marine and terrestrial biomarkers at the onset of the early Aptian oceanic anoxic event 1a: Evidence for the release of13C-depleted carbon into the atmosphere

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scholarly article

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Synchronous negative carbon isotope shifts in marine and terrestrial biomarkers at the onset of the early Aptian oceanic anoxic event 1a: Evidence for the release of13C-depleted carbon into the atmosphere (English)

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Jaap Sinninghe Damsté

object named as

Jaap S. Sinninghe Damsté

6

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Stefan Schouten

2

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Stefan Schouten

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Yvonne van Breugel

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Yvonne van Breugel

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author name string

Harilaos Tsikos

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Elisabetta Erba

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Gregory D. Price

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publication date

23 February 2007

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Paleoceanography

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22

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1

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Global and regional palaeoceanographic changes as recorded in the mid-Cretaceous (Aptian-Albian) sequence of the Ionian zone (NW Greece)

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Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene

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Organic geochemical indicators of palaeoenvironmental conditions of sedimentation

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Leaf epicuticular waxes.

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Evolution patterns of radiolaria and organic matter variations: A new approach to identify sea-level changes in mid-Cretaceous pelagic environments

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Tocopherols as likely precursors of pristane in ancient sediments and crude oils

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Carbon-isotope composition of Lower Cretaceous fossil wood: Ocean-atmosphere chemistry and relation to sea-level change

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Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

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The influence of oxic degradation on the sedimentary biomarker record I: evidence from Madeira Abyssal Plain turbidites

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Terrestrial record of methane hydrate dissociation in the Early Cretaceous

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Evidence for rapid climate change in the Mesozoic–Palaeogene greenhouse world

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Stratigraphy, paleoceanography, and evolution of Cretaceous Pacific guyots; relics from a greenhouse Earth

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Astronomical pacing of methane release in the Early Jurassic period

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Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene

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Diagenetic and catagenetic products of isorenieratene: Molecular indicators for photic zone anoxia

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A thermal and chemical degradation approach to decipher pristane and phytane precursors in sedimentary organic matter

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Interpreting carbon-isotope excursions: carbonates and organic matter

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N2-fixing cyanobacteria supplied nutrient N for Cretaceous oceanic anoxic events

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Comparison of petroleum generation kinetics by isothermal hydrous and nonisothermal open-system pyrolysis

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Changes in carbon dioxide during an oceanic anoxic event linked to intrusion into Gondwana coals

1 reference

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Effects of an oceanic anoxic event on the stable carbon isotopic composition of early Toarcian carbon

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Comments on “Biomarkers or not biomarkers. A new hypothesis for the origin of pristane involving derivation from methyltrimethyltridecylchromans (MTTCs) formed during diagenesis from chlorophyll and alkylphenols” from M. Li, S. R. Larter, P. Tayl

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The identification of mono-, di- and trimethyl 2-methyl-2-(4,8,12-trimethyltridecyl)chromans and their occurrence in the geosphere

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A 6,000-year sedimentary molecular record of chemocline excursions in the Black Sea.

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The influence of oxic degradation on the sedimentary biomarker record II. Evidence from Arabian Sea sediments

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2-Methylhopanoids as biomarkers for cyanobacterial oxygenic photosynthesis

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Release of methane from a volcanic basin as a mechanism for initial Eocene global warming

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Rapid and synchronous collapse of marine and terrestrial ecosystems during the end-Permian biotic crisis

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A kinetic calculation method of homohopanoid maturation: Applications in the reconstruction of burial histories of sedimentary basins

1 reference

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Controls on the molecular and carbon isotopic composition of organic matter deposited in a Kimmeridgian euxinic shelf sea: evidence for preservation of carbohydrates through sulfurisation

1 reference

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Origin and subsidence of Guyots in Mid-Pacific Mountains

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Identifiers

10.1029/2006PA001341

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