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Swiss Geo Web: Das "Who is Who" der Schweizer Geowissenschaften

 

Karl B. Föllmi

Prof. Karl B. Föllmi
Institut de Géologie et de Paléontologie, IGP
Université de Lausanne
Anthropôle
Anthropôle
CH-1015 Lausanne
Switzerland

Phone: +41 (0)21 692 43 63
Phone2: +41 (0)21 692 43 00
Fax: +41 (0)21 692 43 05
E-mail: karl.foellmi@unil.ch
URL: www.unil.ch/igp/

with involvement of Karl B. Föllmi
in which Karl B. Föllmi holds an official function.

Key Publications of Karl B. Föllmi (up to five) :
Föllmi, K.B., Weissert, H., Bisping, M., and Funk, H. (1994). Phosphogenesis, carbon-isotope stratigraphy, and carbonate-platform evolution along the Lower Cretaceous northern tethyan margin. Geological Society of America, Bulletin, v. 106, p. 729-746
Föllmi, K.B. (1995). 160 m.y. record of marine sedimentary phosphorus burial: Coupling of climate and continental weathering under greenhouse and icehouse conditions. Geology, v. 23, p. 859-862.
Föllmi, K.B.(1996). The phosphorus cycle, phosphogenesis, and marine phosphate-rich deposits. Earth-Science Reviews, v. 40, p. 55-124.
Föllmi, K.B., Tamburini, F., Hosein, R., van de Schootbrugge, B., Arn, K., and Rambeau, C. (2004). Phosphorus, a servant faithful to Gaia? Biosphere remediation rather than regulation. In Schneider, S.H.,, Miller, J.R., Crist, E., and Boston, P., eds., Scientists debate Gaia: The Next Century, MIT Press, Cambridge, Massachusetts, p. 79-92.


Expertise of Karl B. Föllmi:
Expertise Category Specific Expertise
Expert TypeScientific / Fundamental Research
Topic LithosphereGeochemical Processes
Sediments: Formation, Dynamics, Metamorphism
Topic Integrated SystemsCarbon Cycle
Biogeochemical Cycles except Carbon
Nutrient Cycle / Food Chain
Time FramePast: Tertiary
Past: Cretaceous
Past: Jurassic
Statistical FocusExtreme Events
Mean Change / Trends
Variability
Time Scale100 kyr
Billenial (Mio yrs)
MethodsData Collection
Data Collection - Measurement
Data Analysis
Literature Study

Additional Specialties:
I am interested in large-scale geochemical processes that modify and are modified by the biosphere in mutual feedback.

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