Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Bas, van de Schootbrugge"'
Autor:
Remco Bos, Wang Zheng, Sofie Lindström, Hamed Sanei, Irene Waajen, Isabel M. Fendley, Tamsin A. Mather, Yang Wang, Jan Rohovec, Tomáš Navrátil, Appy Sluijs, Bas van de Schootbrugge
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-12 (2024)
Abstract The long-term effects of the Central Atlantic Magmatic Province, a large igneous province connected to the end-Triassic mass-extinction (201.5 Ma), remain largely elusive. Here, we document the persistence of volcanic-induced mercury (Hg) po
Externí odkaz:
https://doaj.org/article/d70443a8aa324324bdec19e23e72d8ae
Publikováno v:
Frontiers in Earth Science, Vol 7 (2019)
Preference for certain stable isotopes (isotope fractionation) during enzyme-mediated reactions is a universal aspect of life. For instance, carbon isotopes are fractionated during anabolic (e.g., photosynthate production) and catabolic (e.g., methan
Externí odkaz:
https://doaj.org/article/e581f3da889e47bfb2c28439df304f3d
Autor:
Bas van de Schootbrugge, Martin Schobben, Chloe Morales, Lubos Polerecky, Michiel Kienhuis, Klaas Nierop, Francien Peterse, Nico Janssen, Tianchen He, Rob Newton, Julia van Winden, Johan Weijers, Olaf Podlaha, Appy Sluijs, Jack Middelburg
Fossil ikaite, preserved as the pseudomorph glendonite, occurs in vast amounts in Jurassic and Cretaceous successions in the high Arctic. Thermodynamics predict that ikaite is only stable at near-freezing temperatures and glendonite is thus widely us
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::655db399480df9b40c32a0337936b2df
https://doi.org/10.5194/egusphere-egu23-13182
https://doi.org/10.5194/egusphere-egu23-13182
Glendonites are calcite pseudomorphs after the mineral ikaite. Because ikaite typically forms at low temperature, glendonite occurrences in deep time have been interpreted as indication for cold environmental conditions, even when found in sediments
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f16117d2ec2477a68e7a02e64386308c
https://doi.org/10.5194/egusphere-egu23-15764
https://doi.org/10.5194/egusphere-egu23-15764
The Triassic-Jurassic transition, from the Norian to the Hettangian (corresponding to the Rhaetian), was a critical timespan marked by a series of global environmental perturbations, most notably the end-Triassic mass extinction event (201.6 Ma). Her
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a086197189b03dd301f08e6ba467818a
https://doi.org/10.5194/egusphere-egu23-6742
https://doi.org/10.5194/egusphere-egu23-6742
Autor:
Remco Bos, Sofie Lindström, Johanna van Konijnenburg-van Cittert, Frederik Hilgen, Teuntje P. Hollaar, Hendrik Aalpoel, Carolien van der Weijst, Hamed Sanei, A Rudra, Appy Sluijs, Bas van de Schootbrugge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::362b9c43a92d44b7f935fbec69e732e7
https://doi.org/10.2139/ssrn.4371814
https://doi.org/10.2139/ssrn.4371814
Autor:
Emily Koenders, Pim Kaskes, Niels de Winter, Malte Jochmann, Bas van de Schootbrugge, Martin Ziegler
Publikováno v:
Vrije Universiteit Brussel
Vrije Universiteit Amsterdam
Vrije Universiteit Amsterdam
Glendonites are calcite pseudomorphs, that form after the mineral ikaite. Their occurrence in sediments is typically seen as an indication of cold environmental conditions, even when found in predetermined greenhouse climates (Zhou et al., 2015). How
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::81fe481c0459077241179ce0cc42507d
https://doi.org/10.5194/egusphere-egu22-12047
https://doi.org/10.5194/egusphere-egu22-12047
Autor:
Bas van de Schootbrugge, Sara Callegaro, Andrea Marzoli, Sofie Lindström, Joshua Davies, Gunver Krarup Pedersen, Nasrrddine Youbi, Hamed Sanei, Christian Tegner
Publikováno v:
Lindström, S, Callegaro, S, Davies, J, Tegner, C, Schootbrugge, B V D, Pedersen, G K, Youbi, N, Sanei, H & Marzoli, A 2021, ' Tracing volcanic emissions from the CAMP volcanism in the sedimentary and biotic record ' . https://doi.org/10.5194/egusphere-egu21-10813
The end-Triassic mass extinction (ETME) is thought to have been caused by voluminous, pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last decades, various geochemical signals and proxy records, including δ13C, pC
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::599b5be81b88842ef073ce80b40fd987
https://doi.org/10.5194/egusphere-egu21-10813
https://doi.org/10.5194/egusphere-egu21-10813
The Central Atlantic Magmatic Province (CAMP) eruptions are generally regarded as the main driver of major environmental change and mass-extinction across the Triassic-Jurassic (TJ) boundary (~201.3 Ma), but the exact mechanisms linking volcanism and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3216a186fef27cd55e49accb2753e91d
https://doi.org/10.5194/egusphere-egu21-1069
https://doi.org/10.5194/egusphere-egu21-1069
Autor:
Bas van de Schootbrugge, Wanyi Lu, Zunli Lu, Kimberly V. Lau, Aviv Bachan, Jonathan L. Payne, Pulkit Singh, A. B. Jost
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0df6f122606775084fbe1ae8fdb6641f
https://doi.org/10.1130/abs/2021am-367796
https://doi.org/10.1130/abs/2021am-367796