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All abstracts by Frank Lamy in conference series: Goldschmidt

(2018) Lithium Isotopic Composition of Benthic Foraminifera: A New Proxy for paleo-Ph Reconstruction
Roberts J, Kaczmarek K, Langer G, Skinner L, Bijma J, Bradbury H, Turchyn A, Lamy F & Misra S

(2017) Sources of Glacial South Pacific Dust
Struve T, Wengler M, Lamy F, Winckler G & Pahnke K

(2017) Subantarctic Pacific Iron Fertilization during the Last Ice Age
Martinez-Garcia A, Sigman D, Lamy F, Studer A, Tiedemann R & Haug G

(2017) The Response of the Subantarctic Pacific to Climate Change: Reconstructing Dust Flux and Biological Productivity during the Last Glacial Cycle
Winckler G, Anderson RF, Park J, Schwarz R, Lamp J, Shoenfelt E, Pahnke K, Struve T, Kuhn G, Wengler M & Lamy F

(2016) Abrupt Temperature Changes and Environmental Dynamics in the Black Sea “Lake” during the Last Glacial
Wegwerth A, Kaiser J, Dellwig O, Shumilovskikh LS, Nowaczyk NR, Ganopolski A, Ménot G, Bard E, Lamy F & Arz HW

(2014) Dust in the Southern Hemisphere – From Source to Sink
Winckler G, Borunda A, Koffman B, Recasens C, Pavia F, Kaplan M, Goldstein S, Schwarz R, Anderson R, Lamy F, Gersonde R & Pahnke K

(2011) Is TEX86 Paleothermometry Applicable in the Polar Regions?
Ho SL, Fietz S, Rueda G, Martinez-Garcia A, Mollenhauer G, Rosell-Mele A, Lamy F, Ruggieri N & Tiedemann R

(2009) Are Glacials (Interglacial) in the Easternmost Pacific Ocean Drier (Wetter) during the Last 300 000 Years?
Rincón Martínez D, Contreras S, Lamy F & Tiedemann R

(2009) Plio-Pleistocene Changes in SE Trade Wind Strength and South American Rainfall – Implications for ITCZ Movements and Long-Term El Niño Behavior
Lamy F, Rincon-Martinez D, Saukel C, Steph S, Sturm A, Etourneau J & Tiedemann R

(2000) Coupled Food-Web and Bacterial-Loop Modelling of a Lagrangian Experiment off the Iberian Margin
Soetaert K, Herman P, Middelburg J & Lamy F

(2000) Reconstructing Continental Paleoclimate and Paleoceanographic Changes along the Chilean Continental Margin
Lamy F, Hebbeln D, Rühlemann C & Wefer G

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