Bas van de Schootbrugge
Bas van de Schootbrugge
Bas van de Schootbrugge
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2006:<br />
Palaeoclimatology, Palaeoecology 244, 126-141.<br />
[12] Dunca, E., Doguzhaeva, L., Schöne, B.R., <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong>, B., (2006): Lunar-daily<br />
growth patterns in rostra of the Middle Jurassic belemnite Megateuthis giganteus. Acta<br />
Universitatis Carolinae Geologica, 49. 107-117.<br />
[11] Tremolada, F., Bornemann, A. Bralower, T.J., Koeberl, C. <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong>, B.,<br />
(2006). Paleoceanographic changes across the Jurassic-Cretaceous transition: the<br />
calcareous nannofossil response. Earth and Planetary Science Letters 241: 361-371.<br />
[10] Tremolada, F., Erba, E., <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong>, B., Mattioli, E., (2006). Calcareous<br />
nannofloral changes during the late Callovian-Oxfordian cooling phase. Marine<br />
Micropaleontology 59: 197-209.<br />
[9] Go<strong>de</strong>t, A., Bodin, S., Föllmi, K.B., Vermeulen, J., Gardin, S., Fiet, N., Adatte, T., Berner,<br />
Z., Stüben, D., <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong>, B., (2006). Evolution of the marine stable carbonisotope<br />
record during the early Cretaceous: A focus on the late Hauterivian and<br />
Barremian in the Tethyan realm. Earth and Planetary Science Letters 242: 254-271.<br />
2005:<br />
[8] <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong> B., Bailey, T., Rosenthal, Y., Katz, M.E., Wright, J.D., Feist<br />
Burkhardt, S., Miller, K.G., Falkowski, P.G., (2005). Early Jurassic climate change and<br />
the radiation of organic-walled phytoplankton in the Tethys Ocean. Paleobiology 31: 73-<br />
97.<br />
[7] Tremolada, F., <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong>, B., Erba, E., (2005). The Early Jurassic<br />
Schizosphaerellid crisis in Cantabria, Spain: Implications for calcification rates and<br />
phytoplankton evolution across the Toarcian oceanic anoxic event. Paleoceanography<br />
20: PA2011, doi:10.1029/2004PA001120.<br />
[6] <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong>, B., McArthur, J.M., Bailey, T.R., Rosenthal, Y., Wright, J.D.,<br />
Miller., K.G., (2005). Toarcian Oceanic Anoxic Event: an assessment of global causes<br />
using belemnite carbon isotope records. Paleoceanography 20, PA3008, doi:<br />
10.1029/2004PA001102.<br />
2004:<br />
[5] Föllmi, K.B., Tamburini, F., Hosein, R., <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong>, B., Arn, K., Rambeau, C.<br />
(2004). Phosphorus a ser<strong>van</strong>t faithful to Gaia? Biosphere remediation rather than<br />
regulation. In: S.H. Schnei<strong>de</strong>r, J.R. Miller, E. Crist and P.J. Boston, (Eds.) Scientists on<br />
Gaia: The Next Century, MIT Press, p. 79-92.<br />
[4] Falkowski, P.G., Schofield, O., Katz, M.E., <strong>van</strong> <strong>de</strong> <strong>Schootbrugge</strong>, B., Knoll, A.H., (2004).<br />
Why is the Land Green and the Ocean Red? In: Young, J., Thierstein, H. (Eds.),<br />
Coccolithophorids: from molecular processes to global impact. Elsevier, Amsterdam, p.<br />
429-453.<br />
2003:<br />
3