Magnetotactic bacterial response to Antarctic dust supply during the Palaeocene-Eocene thermal maximum

Autor: Larrasoaña, J.C., Roberts, A.P., Chang, L., Schellenberg, S.A., Fitz Gerald, J.D., Norris, R.D., Zachos, J.C.

Distinct magnetic properties of marine sediments that record the Palaeocene–Eocene thermal maximum (PETM) have been suggested to be due to a bacterial magnetofossil signal that is linked to enhanced weathering conditions during the PETM. We documen

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______101::8646f73560e48ad09b7385ec1e82b06a
https://dspace.library.uu.nl/handle/1874/309730

Rapid acidification of the ocean during the Paleocene-Eocene Thermal Maximum

Autor: Zachos, J.C., Röhl, U., Schellenberg, S.A., Sluijs, A., Hodell, D.A., Kelly, D.C., Thomas, E., Nicolo, M., Raffi, I., Lourens, L.J., McCarren, H., Kroon, D., Palaeobotany and Palynology, The astronomical timescale, Sub AW Personeel 2e geldstroom, Dep Biologie, Stratigraphy and paleontology

Publikováno v: Science, 308, 1611-1615. American Association for the Advancement of Science
Science, 308(5728), 1611. American Association for the Advancement of Science
Zachos, J C, Röhl, U, Schellenberg, S A, Sluijs, A, Hodell, D A, Kelly, D C, Thomas, E, Nicolo, M, Raffi, I, Lourens, L J, McCarren, H & Kroon, D 2005, ' Rapid Acidification of the Ocean During the Paleocene-Eocene Thermal Maximum ', Science, vol. 308, pp. 1611-1615 . https://doi.org/10.1126/science.1109004

The Paleocene-Eocene thermal maximum (PETM) has been attributed to the rapid release of ∼2000 × 10 9 metric tons of carbon in the form of methane. In theory, oxidation and ocean absorption of this carbon should have lowered deep-sea pH, thereby tr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4cc1ceabd1aa0a2251477b4287482abb
https://dspace.library.uu.nl/handle/1874/385806

Eocene circulation of the Southern Ocean: Was Antarctica kept warm by subtropical waters?

Autor: Huber, M., Brinkhuis, H., Stickley, C.E., Döös, K., Sluijs, A., Warnaar, J., Schellenberg, S.A., Williams, G.L., Palaeobotany and Palynology, Universiteit Utrecht, Dep Biologie

Publikováno v: Paleoceanography, 19. American Geophysical Union

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=narcis______::a321252df6d4ff2bbaf8c2f6aebf0c32
https://dspace.library.uu.nl/handle/1874/385798

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