[Thread Prev] | [Thread Next] | [Thread Index] | [Date Prev] | [Date Next] | [Date Index] |
PhD projects in dinoflagellate research Geography Department University of Cambridge, UK APPLICATION DEADLINE APRIL 12 !! (email applications accepted) Two oil industry related topics are available, starting Sept 2002. One is on Late Cenozoic ocean history of the Caribbean Sea, the other on astronomically-calibrated late Cenozoic history of the eastern Mediterranean Sea. Please see below for details, and at the end of this message for directions on how to apply. Funding is available on a competitive basis. The Department has 1 NERC studentship available, but shortlisted candidates from the UK are also recommended for the University's domestic studentship program. Overseas candidates may apply separately for Gates Foundation scholarships (see University website). We welcome enquiries also from those wishing to pursue other Quaternary/Neogene dinoflagellate cyst projects. For more details please see: http://www.geog.cam.ac.uk/research/opportunities/ or contact Martin Head at mh300@cam.ac.uk. Martin. D3. Late Cenozoic ocean history and biostratigraphy of the Caribbean Sea using dinoflagellate cysts (Supervisors: M.J. Head, P.L. Gibbard) The Caribbean Sea region is a major petroleum province but also a key area for understanding the influence of tropical seas on global ocean history and climate evolution. The Caribbean Sea contributes warm, saline waters to the Gulf Stream and is therefore a crucial component of North Atlantic thermohaline circulation. In 1995/1996, the Ocean Drilling Program (ODP) Leg 165 drilled a series of deep sea cores in the Caribbean Sea to assess, among other objectives, the nature of climate change in the region during the late Cenozoic. Leg 165 recovered an essentially complete and now precisely dated Miocene - Holocene record of the Caribbean Sea. Most principal microfossil groups were analyzed for these cores, with the notable exception of dinoflagellates and pollen. Dinoflagellates are sensitive indicators of sea-surface conditions, and the present study will use dinoflagellates to refine the climatic and oceanographic history of the region as well as construct a regional biostratigraphy of economic and academic value. Selected cores will be analyzed for dinoflagellates and pollen to improve understanding of the Plio Pleistocene hydrographic development of the Caribbean Sea, including effects of sea-level fluctuation, and to construct an independently age-constrained dinoflagellate biostratigraphy for the region. ODP Site 1002 (Cariaco Basin) will receive special focus as it contains important varved sequences through the Quaternary that allow millennial-scale changes to be observed. This site has an important oxygen-isotope record characterized by major fluctuations that are caused either by temperature or salinity variations. Dinoflagellates will be used to deconvolute salinity-temperature signals, as well as to assess upwelling and productivity fluctuations. The pollen from this site will be analyzed to assess vegetation development and compare with long terrestrial pollen records available for Venezuela and Columbia. The project is in partnership with BG Group PLC, a major gas producer in the Caribbean region. One or more BG boreholes, located on the Orinoco delta front, offshore Trinidad/Venezuela, will be analyzed for dinoflagellates and pollen, offering an exceptional opportunity to integrate oceanic and terrestrial biostratigraphies for this economically important region. The BG wells are located in a deltaic sediment pile of immense thickness - the Pleistocene alone may be 6.5 km thick. Integrating the sediment and dinoflagellate records may provide clues as to the association of climatically-induced variations in clastic input, and facilitate correlation across this region of repetitive cyclic deposition. Full training in dinoflagellate and pollen analysis will be given in Cambridge, where most of the analysis will be done. Statistical analysis and interpretation of results, including integration with geophysics and seismic stratigraphy, will be undertaken both at Cambridge and during visits to BG Group* at Reading, which will provide regional data, access to state of-the-art stratigraphic/basin analysis techniques and software and promote an awareness of the industrial application of results. * Pending final approval from BG Group. D4. Astronomically-calibrated late Cenozoic history and biostratigraphy of the eastern Mediterranean Sea using dinoflagellate cysts (Supervisors: M.J. Head, P.L. Gibbard) The eastern Mediterranean Sea was drilled in 1995 by the Ocean Drilling Program (ODP) during Leg 160 in order to elucidate, among other objectives, the palaeoceanographic history of the region. A particular focus was on the origin and significance of sapropels (organic-rich layers) that occur through the Pliocene and Quaternary of the Mediterranean. These sapropels sensitively record the control of orbitally-driven climate change on sedimentation. They provide, in conjunction with colour cycles, oxygen isotopes and mineralized microfossils, a highly precise astronomically-tuned geochronology for these sediments. The project will investigate the dinoflagellate and acritarch record of these Pliocene and Quaternary sediments of the eastern Mediterranean, which exceed 100 m at the following ODP Leg 160 sites: 966 (plateau top of Eratosthenes Seamount), 967 (northern slope of Eratosthenes Seamount), 968 (Cyprus margin), and 969 (Mediterranean Ridge). Dinoflagellates and acritarchs will be used to construct a basin-wide dinoflagellate ecostratigraphy, to improve understanding of salinity and temperature fluctuations in surface waters during and between sapropel formation, and to test for any evidence of upwelling during sapropel formation. Results will be compared with detailed stable isotope and alkenone data already published for these cores. Sediments will be analysed also for pollen where appropriate. The project is in partnership with BG Group PLC which has a successful record of drilling in the eastern Mediterranean region. One or more BG boreholes from offshore Gaza and Israel will be analysed for dinoflagellates and pollen, with the aim of improving biostratigraphic resolution by application of the ODP-based dinoflagellate record. These boreholes complete an E-W transect through the eastern Mediterranean, and provide an important opportunity to integrate oceanic and terrestrial biostratigraphies for this economically important region. Full training in dinoflagellate and pollen analysis will be given in Cambridge, where most of the analysis will be done. Statistical analysis and interpretation of results, including integration with extensive 3D seismic data, will be undertaken both at Cambridge and during visits to the BG Group* at Reading, which will provide regional data, access to state-of-the art stratigraphic/basin analysis techniques and software and promote an awareness of the industrial application of results. * Pending final approval from BG Group. HOW TO APPLY All applications should be made via e-mail attachments or in writing to: Dr. Ian Willis c/o The Graduate School Department of Geography University of Cambridge Downing Place Cambridge CB2 3EN UK (Tel: 01223 333375) (Fax: 01223 333392) (e-mail: iw102@cus.cam.ac.uk) In your e-mail attachment or letter, please indicate the research project (or projects) you are interested in, the reasons for this preference, and the expertise you would bring to the project(s). Please include a curriculum vitae together with the names and e-mail addresses of two referees. The closing date for applications is Friday 12 April 2002 --------------------------------------------------------------------- Martin J. Head Senior Research Associate, and Visiting Fellow of Wolfson College Godwin Institute for Quaternary Research Department of Geography University of Cambridge Downing Place, Cambridge CB2 3EN ENGLAND, U.K. Phone: (01223) 339751 Fax: (01223) 333392 Email: mh300@cam.ac.uk Home page: http://www.cus.cam.ac.uk/~mh300 ======================================================================
Partial index: