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G. J. de Lange

Researcher at Utrecht University

Publications -  92
Citations -  6612

G. J. de Lange is an academic researcher from Utrecht University. The author has contributed to research in topics: Sapropel & Water column. The author has an hindex of 45, co-authored 92 publications receiving 6204 citations.

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Selective preservation of organic matter in marine environments; processes and impact on the sedimentary record

TL;DR: The main theme of the workshop as discussed by the authors was to understand the impact of selective degradation/preservation of organic matter (OM) in marine sediments on the interpretation of the fossil record, including the influence of the molecular composition of OM in relation to the biological and physical depositional environment, including new methods for determining complex organic biomolecules.
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Magnetostratigraphy and astronomical calibration of the last 1.1 Myr from an eastern Mediterranean piston core and dating of short events in the Brunhes

TL;DR: In this article, a 37 m long piston core (KC-O1B) was collected from the Calabrian Ridge in the Ionian Sea, and the authors used the oxygen isotope data as an additional constraint on their age model.
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Redistribution and geochemical behaviour of redox-sensitive elements around S1, the most recent eastern Mediterranean sapropel

TL;DR: In this article, the distribution of redox-sensitive elements above, in and below the sharply defined, organic-rich unit reveal that S 1 has already suffered heavy diagenetic alteration.
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Post-depositional stability of long-chain alkenones under contrasting redox conditions

TL;DR: In this article, the long-chain alkenone composition of sediment samples from above and below an oxidation front in an ungraded turbidite layer in the Madeira Abyssal Plain was analyzed to evaluate the postdepositional stability of these biomarkers under contrasting redox conditions.
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Active post-depositional oxidation of the most recent sapropel (S1) in sediments of the eastern Mediterranean Sea

TL;DR: In this paper, a barium-organic carbon relationship is used to calculate the initial organic carbon profile of the S1 sapropel and the palaeoproductivity profiles generated by this method demonstrate that the original sapropels unit was bounded by the upper Mn peak.