
I am a paleoclimatologist/marine geologist who
studies the history and causes of climate change in the Earth's past. This page
provides links to my current research, publications, and published data sets, as
well as other science-related material. The National Science Foundation has
funded much of this research and their support is gratefully acknowledged*. If
you are a student interested in the uplift-weathering hypothesis click here.
If you have difficulty viewing any part of this web site or have questions
about any data or papers, please contact me at raymo(at)ldeo.columbia.edu.
I am currently looking for talented motivated graduate students and/or
post-docs to work on projects related to Pliocene sea level as well as Laurentide and Antarctic ice sheet history over the late
Pliocene to early Pleistocene. Our paper "Plio-Pleistocene
ice volume, Antarctic climate, and the global d18O record"
published in 2006 discusses one problem I continue to investigate. Our recent
paper "Departures from eustasy in Pliocene
sea-level records" discusses our PLIOMAX sea level project. You can
download these papers by following links on my Publications page. On-line application for post-doctoral
positions can be found here.
Three Post-Doctoral Research
Scientists in Paleoclimatology and Paleoceanography:
The Lamont-Doherty Earth Observatory of Columbia University
invites applications for three full-time post-doctoral research scientist
positions in the field of paleoclimatology and paleoceanography. The successful candidates will join a
dynamic and interdisciplinary group of scientists working on a wide range of
interrelated problems examining past climate history, ocean chemistry and
circulation, ice sheet stability, sea level, and the interactions of the solid
Earth, ocean, and cryosphere. The positions are
full-time 1-year appointments, with the opportunity for continuation and growth
depending on progress and availability of funding.
We seek
qualified, highly motivated candidates for the following research activities:
o Past sea level changes. The successful candidate will undertake
field work and related analyses leading to a better
understanding of Plio-Pleistocene sea level history. This work will be part of the larger
collaborative PLIOMAX project, and target locations in the circum-Indian and
Atlantic Ocean regions; field experience and dating expertise in
carbonate sedimentary environments and coral reef ecology and structure is
essential.
Contact:
Maureen Raymo (raymo@ldeo.columbia.edu)
o Sediment geochemistry.
The successful candidate will investigate the history of the Laurentide ice sheet over the Plio-Pleistocene
through analysis of Gulf of Mexico sediment cores; investigation of multiple
proxies and innovative application of new proxies to core material is
anticipated; expertise in foram geochemistry, clay
mineralogy and/or XRF techniques desirable.
Contact: Maureen Raymo (raymo@ldeo.columbia.edu)
o Foraminifer shell geochemistry/paleoceanographer. The successful candidate will work on
one of several potential research areas including coretop
calibrations of planktonic foraminifera and pteropods with oceanic carbon chemistry and physical
parameters, Pliocene changes in the composition and ventilation of upper ocean waters,
and high-resolution records of Holocene SST variability. The candidate will
have experience with species identification, stable isotope geochemistry and
analysis, and trace element analyses using ICP-MS (mid-2012 delivery).
Contact
Peter deMenocal (peter@ldeo.columbia.edu)
*Required disclaimer: Any opinions, findings, and conclusions or
recommendations expressed in this material are those of the author and do not
necessarily reflect the views of the National Science Foundation.
