- Acronym
- AISDy
- Code
- PNRA18_00233
- Anno
- 2018
- Research area
- Earth science
- Specific research topic
- Interazione tra processi glaciali, processi sedimentari ed evoluzione climatica
- Region of interest
- Central Ross Sea
- PI
- Matteo Perotti
- PI establishment
- Università di Siena
- Institutional website
- https://www.dsfta.unisi.it/it
- Other institutions and subjects involved
- Università di Trieste, CNR-IGG, Università di Padova
- Consistency of the research team
- Project status
- In progress
- Main stations used
- Attività svolta in Italia
- The project
IODP Exp.374 recently recovered high quality cores in five sites on the Ross Sea continental shelf, slope, and rise to improve understanding of the sensitivity of the Antarctic Ice Sheets (and particularly the West Antarctic Ice Sheet - WAIS) to past climatic and oceanic conditions, especially during warmer-than-present climate. The co-proponents of this proposal have been selected and approved as shore-based Science Team members. In addition, the science team in this proposal recognize as important the study of correlative core sections from already cored drill-holes South and North of the IODP sites. Therefore some methodologies, including detailed petrology of granule to cobble size clasts analyses, AFT, U-Pb dating of detrital apatite and zircons are proposed to be extended to clast and sand-grains rich intervals in DSDP Leg 28 cores. The integration of these data with the IODP ones (this latter constituting the core portion of the studied materials) will help in better constrain ice flow modelling based on several provenance tools. The project is based on the application of a multi-disciplinary approach including; ostracod analysis, their C-O stable isotope analysis, clast petrography and petrology, and, limited to DSDP cores, also on combined detrital thermochronology and geochronology.
- Images
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- Motivation, importance of research
Core and log data from a transect of six sites with cores recovered by the IODP 374 from the outer continental shelf to rise in the eastern Ross Sea (Preliminary Report, IODP EXP. 374, 2018) can be used to: (1) evaluate WAIS contribution to far-field ice volume and sea level estimates; (2) reconstruct ice proximal atmospheric and oceanic temperatures to identify periods of past polar amplification and assess forcing/feedbacks; (3) assess the role of oceanic forcing (e.g., sea level, temperature) on WAIS instability; (4) document WAIS sensitivity to Earth’s orbital configuration under varying climate boundary conditions; and (5) reconstruct eastern Ross Sea bathymetry to examine relationships among seafloor geometry, ice sheet instability, and global climate.
- Objectives of the proposal
- Activities carried out and results achieved
- Products