H
Hubert B. Vonhof
Researcher at Max Planck Society
Publications - 116
Citations - 3262
Hubert B. Vonhof is an academic researcher from Max Planck Society. The author has contributed to research in topics: Geology & Speleothem. The author has an hindex of 30, co-authored 92 publications receiving 2697 citations. Previous affiliations of Hubert B. Vonhof include VU University Amsterdam & University of Bremen.
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Fossil dripwater in stalagmites reveals Holocene temperature and rainfall variation in Amazonia
M. R. van Breukelen,M. R. van Breukelen,Hubert B. Vonhof,John Hellstrom,W. C. G. Wester,Dirk Kroon +5 more
TL;DR: In this article, the coupled isotope composition of fossil dripwater trapped in stalagmite fluid inclusions, and that of the calcite hosting the fluid-inclusions, was used to calculate independent paleotemperatures and rainfall amounts.
Lake Pebas: a palaeoecological reconstruction of a Miocene, long-lived lake complex in western Amazonia
Frank P. Wesselingh,Matti Räsänen,Georg Irion,Hubert B. Vonhof,R.J.G. Kaandorp,Willem Renema,L. Romero Pittman,Murray K. Gingras +7 more
TL;DR: The taxonomic composition and palaeoecological signature of molluscan faunas from the Miocene Pebas Formation of Peruvian Amazonia are assessed in this paper.
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Speleothem record of the last 180 ka in Villars cave (SW France): Investigation of a large δ18O shift between MIS6 and MIS5
K. Wainer,K. Wainer,Dominique Genty,Dominique Blamart,M. Daëron,Miryam Bar-Matthews,Hubert B. Vonhof,Yuri Dublyansky,Edwige Pons-Branchu,L. E. Thomas,P. van Calsteren,Yves Quinif,Nicolas Caillon +12 more
TL;DR: The Vil-car-1 flowstone core from Villars cave (SW France) provides one of the first European speleothem records extending back to 180 ka, based on UeTh TIMS and MC-ICP-MS measurements as mentioned in this paper.
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Global cooling accelerated by early late Eocene impacts
TL;DR: In this article, δ18O records of fine-fraction bulk carbonate and benthic foraminifers indicate that accelerated climate cooling took place following at least two closely spaced early late Eocene extraterrestrial impact events.
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Reconstruction of the Miocene western Amazonian aquatic system using molluscan isotopic signatures.
TL;DR: Strontium isotopic ratios and Sr contents of molluscs from the Miocene Pebas Formation in Colombian Amazonia indicate that the bulk of the Pebas formation was deposited in a freshwater environment, predominantly draining the Andes, with minor contribution from the shield regions as mentioned in this paper.