Bas van de Schootbrugge

Bas van de Schootbrugge
Institute of Geosciences
Johann Wolfgang Goethe University Frankfurt
Altenhöferallee 1
D – 60438 Frankfurt am Main, Germany
phone: ++49 (0)69 798 40178
fax: ++49 (0)69 798 40185
email: van.de.Schootbrugge@em.uni-frankfurt.de
http://www.geologie.uni-frankfurt.de/staff/homepages/schootbrugge.html
Born: April 5, 1973 in Utrecht, The Netherlands
Nationality: Dutch
EMPLOYMENT:
2007 – present „Akademischer Rat“, Institute of Geosciences, Goethe University
Frankfurt, Germany
2005 – 2007 „Wissenschaftlicher Angestellter“, Institute of Geosciences, Goethe
University Frankfurt, Germany
2002 – 2005 Postdoctoral Researcher, Institute of Marine and Coastal Sciences,
Rutgers University, New Jersey, USA
1997 – 2001 Doctoral Research Assistant, Institute of Geosciences, University of
Neuchâtel, Switzerland
ACADEMIC EDUCATION:
2001 Ph.D., University of Neuchâtel, Switzerland
Thesis title: „Influence of paleo-environmental changes during the
Hauterivian on carbonate deposition along the northern margin of the
Tethys: evidence from stable isotopes (C,O,Sr) and trace elements (Fe,
Mn, P)“.
Advisor: Karl B. Föllmi
1997 M.Sc. University of Utrecht, The Netherlands
Thesis title: „Palynology and stable isotopes of the Permian-Triassic
boundary in the Montan section, Western Dolomites, Italy “
Advisor: H. Visscher
STIPENDS AND AWARDS:
2008 „Blaustein Visiting Professor“, Stanford University, Palo Alto, USA
2002 – 2003 Postdoctoral stipend, Swiss National Science Foundation
2001 Prix-academique „Best doctoral thesis in paleontology“, University of
Neuchâtel, Switzerland
OTHER PROFESSIONAL EXPERIENCE:
Proposal Peer-Reviewer: National Science Foundation (USA), German Science
Foundation (DFG)
Paper Peer-Reviewer: Nature, Nature Geoscience, Newsletters on Stratigraphy, Palaeo-3,
Earth and Planatery Science Letters, Chemical Geology, Sedimentology, Paleobiology,
Paleoceanography, Cretaceous Research, Geological Society of London.
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MEMBERSHIPS:
American Geophysical Union AGU, Symbiosis Society, Geological Society of America GSA
PUBLICATIONS (ISI Journals in bold):
In press and submitted:
[23] van de Schootbrugge, B., Quan, T., Lindström, S., Pross, J., Fiebig, J., Petschick, R.,
Püttmann, W., Rosenthal, Y. & Falkowski, P.G, subm.: Acid rain and the demise of
terrestrial ecosystems at the Triassic-Jurassic boundary. Nature Geoscience
[22] McArthur, J.M., Algeo, T., van de Schootbrugge, B., Li, Q., Howarth, R.J., in review.:
Basin restriction, the formation of black shales, and the Early Toarcian Oceanic Anoxic
Event. Paleoceanography
[21] Kotthoff, U., Müller, U.C., Pross, J., Schmiedl, G., van de Schootbrugge, B., Lawson, I. &
Schulz, H., in press: Lateglacial and Holocene vegetation dynamics in the Aegean
region: An integrated view based on pollen data from marine and terrestrial archives.
The Holocene.
[20] van de Schootbrugge, B., Payne, J.L., Tomasovych, A., Pross, J., Fiebig, J., Benbrahim,
M., Föllmi, K.B., & Quan, T.M., (2008) Carbon cycle perturbation and stabilisation in the
wake of the Triassic-Jurassic boundary mass-extinction event. Geochemistry
Geophysics Geosystems.
[19] Stanley Jr., G.D., van de Schootbrugge, B., in press: Evolution of the coral-algal
symbiosis in scleractinians. In: Lough, J., van Oppen, M. (Eds.), Coral bleaching:
Patterns, Processes, Causes and Consequences. Springer Ecological Studies.
[18] Godderis, Y., Donnadieu, Y., de Vargas, C., Pierrehumbert, R.T., Dromart, G., & van de
Schootbrugge, B. (2008): Causal or casual link between the rise of nannoplankton
calcification and a tectonically-driven massive fall of atmospheric CO2? Earth and
Planetary Science Letters 267, 247-255.
[17] Quan, T., van de Schootbrugge, B., Field, P.M., Rosenthal, Y. & Falkowski, P.G., (2008).
Nitrogen isotope and trace metal analyses from the Mingolsheim core (Germany):
Evidence for redox variations across the Triassic-Jurassic boundary. Global
Biogeochemical Cycles.
2007:
[16] McArthur, J.M., Janssen, N.M.M., Leng, M.J., Reboulet, S., Thirlwall, M.F., van de
Schootbrugge, B., (2007). Palaeo-temperatures, polar ice-volume, and isotope
stratigraphy (Mg/Ca, δ 18 O, δ 13 87 86
C, Sr/ Sr): the Early Cretaceous (Berriasian,
Valanginian, Hauterivian). Palaeogeography, Palaeoclimatology, Palaeoecology 248:
391-430.
[15] Payne, J.L., van de Schootbrugge, B. (2007). Ocean life in the Triassic: Links between
benthic and planktonic recovery and radiation. In: Falkowski, P.G., Knoll, A.H. (Eds.),
Evolution of Primary Producers in the Sea, Elsevier, Amsterdam, p. 165-189.
[14] Föllmi, K.B., Bodin, S., Godet, A. Linder, P., van de Schootbrugge, B. (2007). Unlocking
paleo-environmental information from early Cretaceous shelf sediments in the helvetic
Alps: stratigraphy is the key! Swiss Journal of Geosciences DOI 10.1007/s00015-007-
1236-
[13] van de Schootbrugge, B., Tremolada, F., Rosenthal, Y., Bailey, T.R., Feist-Burkhardt, S.,
Brinkhuis, H., Pross, J., Kent, D.V. & Falkowski, P.G., 2007: End-Triassic calcification
crisis and blooms of organic-walled “disaster species”. Palaeogeography,
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2006:
Palaeoclimatology, Palaeoecology 244, 126-141.
[12] Dunca, E., Doguzhaeva, L., Schöne, B.R., van de Schootbrugge, B., (2006): Lunar-daily
growth patterns in rostra of the Middle Jurassic belemnite Megateuthis giganteus. Acta
Universitatis Carolinae Geologica, 49. 107-117.
[11] Tremolada, F., Bornemann, A. Bralower, T.J., Koeberl, C. van de Schootbrugge, B.,
(2006). Paleoceanographic changes across the Jurassic-Cretaceous transition: the
calcareous nannofossil response. Earth and Planetary Science Letters 241: 361-371.
[10] Tremolada, F., Erba, E., van de Schootbrugge, B., Mattioli, E., (2006). Calcareous
nannofloral changes during the late Callovian-Oxfordian cooling phase. Marine
Micropaleontology 59: 197-209.
[9] Godet, A., Bodin, S., Föllmi, K.B., Vermeulen, J., Gardin, S., Fiet, N., Adatte, T., Berner,
Z., Stüben, D., van de Schootbrugge, B., (2006). Evolution of the marine stable carbonisotope
record during the early Cretaceous: A focus on the late Hauterivian and
Barremian in the Tethyan realm. Earth and Planetary Science Letters 242: 254-271.
2005:
[8] van de Schootbrugge B., Bailey, T., Rosenthal, Y., Katz, M.E., Wright, J.D., Feist
Burkhardt, S., Miller, K.G., Falkowski, P.G., (2005). Early Jurassic climate change and
the radiation of organic-walled phytoplankton in the Tethys Ocean. Paleobiology 31: 73-
97.
[7] Tremolada, F., van de Schootbrugge, B., Erba, E., (2005). The Early Jurassic
Schizosphaerellid crisis in Cantabria, Spain: Implications for calcification rates and
phytoplankton evolution across the Toarcian oceanic anoxic event. Paleoceanography
20: PA2011, doi:10.1029/2004PA001120.
[6] van de Schootbrugge, B., McArthur, J.M., Bailey, T.R., Rosenthal, Y., Wright, J.D.,
Miller., K.G., (2005). Toarcian Oceanic Anoxic Event: an assessment of global causes
using belemnite carbon isotope records. Paleoceanography 20, PA3008, doi:
10.1029/2004PA001102.
2004:
[5] Föllmi, K.B., Tamburini, F., Hosein, R., van de Schootbrugge, B., Arn, K., Rambeau, C.
(2004). Phosphorus a servant faithful to Gaia? Biosphere remediation rather than
regulation. In: S.H. Schneider, J.R. Miller, E. Crist and P.J. Boston, (Eds.) Scientists on
Gaia: The Next Century, MIT Press, p. 79-92.
[4] Falkowski, P.G., Schofield, O., Katz, M.E., van de Schootbrugge, B., Knoll, A.H., (2004).
Why is the Land Green and the Ocean Red? In: Young, J., Thierstein, H. (Eds.),
Coccolithophorids: from molecular processes to global impact. Elsevier, Amsterdam, p.
429-453.
2003:
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[3] Bailey, T.R, Rosenthal, Y., McArthur, J.M., van de Schootbrugge, B., Thirlwall, M.F.,
(2003). Paleoceanographic changes of the Late Pliensbachian - Early Toarcian interval:
a possible link to the genesis of an Oceanic Anoxic Event. Earth and Planetary
Science Letters 212: 307-320.
[2] van de Schootbrugge, B., Kuhn, O., Adatte, T., Steinmann, P., Föllmi, K.B., (2003).
Decoupling of P- and Corg burial following Early Cretaceous (Valanginian-Hauterivian)
platform drowning along the NW Tethyan margin. Palaeogeography,
Palaeoclimatology, Palaeoecology 199: 315-331.
2000
[1] van de Schootbrugge, B., K.B. Föllmi, L.G. Bulot, and S.J. Burns, (2000).
Paleoceanographic changes during the early Cretaceous (Valanginian-Hauterivian):
evidence from oxygen and carbon stable isotopes. Earth and Planetary Science
Letters 181: 15-31.
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