Skip to main content
Go to the home page of the European Commission (opens in new window)
English en
CORDIS - EU research results
CORDIS

Testing solid earth climate connections through mid ocean ridge time series

Project description

Quantifying feedback between climate variations and solid Earth processes

The ERC-funded T-SECTOR project will test the possible connections between climate change over glacial cycles and the formation of the ocean floor through integrated geochemical, petrological and geophysical studies. The effect of sea level variations associated with glacial-interglacial periods on volcanism at mid-ocean spreading centres – where oceanic plates are formed – will be quantified. This will be achieved by integrating time series of crustal thickness, hydrothermal activity and glass chemistry in relation to sea level changes. Three study sites in the Atlantic and Pacific Oceans representing different spreading rates will allow the comparison of these systems. Such time series open up a new dimension to ocean ridge research and enable rigorous testing of hypotheses linking volcanism and climate change at mid-ocean ridges.

Objective

A central problem of understanding the Earth system is quantifying climate-solid Earth feedback that requires time-series studies. One important time series is the climate (sea level) record that shows transitions between ice ages and warm periods for the last millions of years, involving vast mass transfer between continents (ice load) and oceans. Volcanism is sensitive to such pressure changes, but its response to glacial cycles is largely unknown for the global mid-ocean-ridge (MOR) system, where 80% of Earth’s volcanism occurs. Models of MOR response to sealevel fluctuations predict changes in crustal thickness, chemistry of lavas and hydrothermal activity. Establishing high-resolution time series on MORs, however, has previously not been possible, because the sea floor is rapidly covered by sediment as it moves away from the MOR and thus cannot be directly sampled. Recent studies, however, show MOR eruptions deposit samples of lava as glass on nearby sediments for up to 100 ka. These carbonate-rich sediments can be precisely dated by oxygen isotope stratigraphy and provide an archive of ridge eruptions (glasses) and hydrothermal activity (trace metals) in the sediments that can be sampled by gravity coring. Through closely spaced new cores to be retrieved during multiple research cruises, a high-resolution time series of volcanism and hydrothermal activity can be achieved and directly linked to the climate record, whereas seismic techniques can be used to determine variations in crustal thickness over time. We propose to obtain integrated data sets for all these processes from slow, intermediate and fast spreading ridge segments over the past 1.5 Ma in unprecedented detail. The results of these glass, sediment and crustal thickness time series will allow us to unequivocally test the influence of glacial cycles on MOR processes and will provide the first high-resolution time series of ocean ridge magmatism, opening up a new frontier of scientific exploration.

Fields of science (EuroSciVoc)

Keywords

Programme(s)

Topic(s)

Funding Scheme

HORIZON-ERC-SYG - HORIZON ERC Synergy Grants

See all projects funded under this funding scheme

Call for proposal

(opens in new window) ERC-2022-SYG

See all projects funded under this call

Host institution

HELMHOLTZ-ZENTRUM FUR OZEANFORSCHUNG KIEL (GEOMAR)
Net EU contribution
€ 11 475 220,00
Address
WISCHHOFSTRASSE 1-3
24148 Kiel
Germany
Region
Schleswig-Holstein Schleswig-Holstein Kiel, Kreisfreie Stadt
Activity type
Research Organisations
Links
Total cost
€ 11 475 220,00

Beneficiaries (3)