CACH

Reconstructing abrupt Changes in Chemistry and Circulation of the Equatorial Atlantic Ocean: Implications for global Climate and deep-water Habitats

 Coordinatore UNIVERSITY OF BRISTOL 

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 Nazionalità Coordinatore United Kingdom [UK]
 Totale costo 1˙998˙833 €
 EC contributo 1˙998˙833 €
 Programma FP7-IDEAS-ERC
Specific programme: "Ideas" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013)
 Code Call ERC-2011-StG_20101014
 Funding Scheme ERC-SG
 Anno di inizio 2011
 Periodo (anno-mese-giorno) 2011-10-01   -   2017-09-30

 Partecipanti

# participant  country  role  EC contrib. [€] 
1    UNIVERSITY OF BRISTOL

 Organization address address: TYNDALL AVENUE SENATE HOUSE
city: BRISTOL
postcode: BS8 1TH

contact info
Titolo: Dr.
Nome: Laura Frances
Cognome: Robinson
Email: send email
Telefono: +44 117 3315158

UK (BRISTOL) hostInstitution 1˙998˙833.00
2    UNIVERSITY OF BRISTOL

 Organization address address: TYNDALL AVENUE SENATE HOUSE
city: BRISTOL
postcode: BS8 1TH

contact info
Titolo: Ms.
Nome: Audrey
Cognome: Michael
Email: send email
Telefono: +44 117 3317371
Fax: +44 117 9250900

UK (BRISTOL) hostInstitution 1˙998˙833.00

Mappa


 Word cloud

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archives    samples    deep    equator    nutrients    coral    heat    geochemical    chemistry    corals    sea    gaps    climate    skeletons    atlantic    ocean    past   

 Obiettivo del progetto (Objective)

'Ice-core records show that glacials had lower atmospheric pCO2 and cooler temperatures than today and that the last deglaciation was punctuated by large, abrupt millennial-scale climate events. Explaining the mechanism controlling these oscillations remains an outstanding puzzle. The ocean is a key player, and the Atlantic is particularly dynamic as it transports heat, carbon and nutrients across the equator. This project proposes to consolidate my research through a focused study of present and past ocean chemistry in the Equatorial Atlantic and to assess the impact of ocean chemistry on fragile deep-sea ecosystems. Despite decades of research there are distinct gaps in our knowledge of the history of the deep and intermediate ocean. Major hurdles include access to suitable archives, development of geochemical proxies and analyses that are sufficiently precise to test climate hypotheses. Through a combination of ship board field work, modern calibrations and cutting-edge geochemical analyses this project will produce samples and data that address each of these gaps. A particular focus will be on using the skeletons of deep-sea corals. Research using deep-sea corals as climate archives, and indeed research into their habitats, environmental controls and potential threats to their survival are still fields in their infancy. The expense and logistics of working in the deep ocean, the complexity of the ecosystem and the biogeochemistry of the coral skeletons have all proved to be significant challenges. The potential payoffs of high-resolution, dateable archives, however, make the effort worthwhile. There have been no studies that attempt to match up co-located deep-sea coral, seawater and sediment samples in a single program, so this would be the first directed study of its type, and as such promises to provide a substantial step in quantifying the fluxes and transport of mass, heat and nutrients across the equator in the past.'

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