
The successful candidates must be in place by June 2010 so that they may join in the first network activity.
Applicants must meet the eligibility and mobility requirements for the European Commission Framework 7 Marie Curie Actions
For more information, please download a detailed description of the projects, or contact the appropriate lead institution.
The ESRs will be members of our team executing research on palaeoceanographic change in the Indonesian Throughflow (ITF) area on orbital timescales that allow integration of biotic evolution, ocean chemistry and circulation changes. Specific objectives include:
ns) One ESR will (1) Quantify the changes in large benthic foraminifera (LBF) assemblage composition with time, and (2) produce a detailed map of external and internal morphospace occupied by LBF. Secondary goals, in cooperation with other projects, will be to place these in a highly resolved chronostratigraphic and environmental framework.
A second ESR will study the development of and turnover in shallow marine mollusk communities during the Oligocene and Neogene in order to understand the emergence of modern communities. The palaeocommunities include mangrove, estuarine as well as seagrass faunas. The research is taxonomy and taphonomy based and includes multivariate numerical approaches.
Two ESRs will be hired by the NHM as part of the Biodiversity Work Package. One will work on fossil reef-corals and the second will work with fossil bryozoans, and both will be responsible for documenting the Cenozoic history of taxa in SE Asia using a specimen-based approach combined with taxonomic revision of one or more key clades within they group. In particular, the aim to is to determine the timing of origin of the modern-day center of marine biodiversity and to document regional response to Cenozoic environmental change resulting from constriction of the Indonesian Throughflow.
The research project at RHUL will focus on extracting reliable palaeoclimate / palaeoceanographic proxy data using (isotope) geochemical techniques. Specifically, well-preserved molluscs, corals and foraminifera will be utilized to reconstruct past sea-surface temperatures (SST), sea-surface salinity (SSS), variations in riverine runoff, or palaeo-pH. These environmental data will be used to reconstruct local environmental change associated with both global changes and regional factors related to the evolution of the Indonesian Throughflow.
The ESR will explore the influence of tectonic changes (e.g., Australian Plate drift, closure of the Tethys Seaway) on the Indonesian Throughflow (ITF) by means of climate modeling. The role of ITF changes in shaping the global ocean circulation and its influence on climate will be studied using the comprehensive Community Climate System Model, version 3 (CCSM3). To this end, the climate model will be set up with paleogeographic configurations based on plate tectonic reconstructions for Oligocene-Miocene time slices.
The ESR that will be hired by the Utrecht University will work on the construction of a chronostratigraphic framework for the Oligocene-Miocene successions of SE Asia by applying integrated stratigraphic dating techniques such as magnetostratigraphy, radiometric dating and isotope stratigraphy.