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| Author(s): |
Daniel Rodelli
Total Authors: 1
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| Document type: | Doctoral Thesis |
| Press: | São Paulo. |
| Institution: | Universidade de São Paulo (USP). Instituto Oceanográfico (IO/DIDC) |
| Defense date: | 2018-09-12 |
| Examining board members: |
Luigi Jovane;
Jairo Francisco Savian;
Felipe Antonio de Lima Toledo;
Ricardo Ivan Ferreira da Trindade
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| Advisor: | Luigi Jovane |
| Abstract | |
The climatic history of the planet Earth is characterized by long- and short-term climatic variations. Oxygen isotopic data clearly shows how during the Cenozoic (from 65 Ma to the present) our planet shifted over time, from greenhouse to icehouse climate states up to the present. Along this progressive cooling, the record is dotted by rapid warming and cooling transient events, from which the causes are not yet fully understood. One problem with paleoceanographic reconstructions is that the older the event, the harder it is to find a sedimentary record in which the paleoclimatic proxies are preserved enough to be used with confidence. This work has the goal of illustrating the possibility to develop a new paleoenvironmental indicator based on the magnetic properties of magnetite crystals synthetized by magnetotactic bacteria. The sensibility of such crystals to small changes in dissolved oxygen content in the pore water and water column is well known, and can be exploited to reconstruct such changes from the sedimentary record. Qualitative information regarding this topic are defined in scientific literature, but, so far, no quantitative study has been performed. This is the first attempt to quantify the preservation of biogenic magnetite as a function of oxygenation state of waters, and is based on recent sediment extracted from cores collected in the coastal region of Rio de Janeiro (Saco do Mamanguá, Paraty). From these, where it was possible to obtain magnetic data relative to magnetite crystals together as well with as direct measurements of pore water chemistry. The results of this first attempt were used to analyze climatic and oceanographic conditions in two other sites, representative of key past environmental events during the Paleocene. The first case study was performed in a newly descripted sedimentary outcrop in central Turkey, of middle Eocene age, representative of a period of rapid warming (Middle Eocene Climatic Optimum, MECO). The second case study was done using material from a marine sediment core collected in the Ross Sea (Antarctica) that covers from the late Eocene to the Middle Miocene, a period that saw the onset of the modern, permanent ice sheet cover in the Antarctic continent. (AU) | |
| FAPESP's process: | 12/21212-3 - Unravel middle Eocene-Oligocene paleoclimate and paleoceanography using paleomagnetism |
| Grantee: | Daniel Rodelli |
| Support Opportunities: | Scholarships in Brazil - Doctorate |