Substantial and correlated changes in marine carbonate (CaCO3) content
of oceanic sediments commonly accompany the transitions from cold glacial periods to warm interglacial periods.
Not exact matches
Sediment - covered basalt on the flanks
of mid-ocean ridges constitutes most
of Earth's
oceanic crust, but the composition and metabolic function
of its microbial ecosystem are largely unknown.
Records
of sea surface temperature from
oceanic sediment cores, for example, show that the magnitude
of warming following several previous glaciations are well - correlated (www.ncdc.noaa.gov/paleo/recons.html).
With the
oceanic plate, water enters the earth as it is trapped in minerals
of the
oceanic crust or overlaying
sediments.
Carbonates are important constituents
of marine
sediments and are heavily involved in the planet's deep carbon cycle, primarily due to
oceanic crust sinking into the mantle, a process called subduction.
An abrupt warming
of oceanic intermediate waters could have initiated the thermal destabilization
of sediment - hosted methane gas hydrates and potentially triggered
sediment slumps and slides.
Researchers from the Centre for Arctic Gas Hydrate, Environment and Climate (CAGE) at the Arctic University
of Norway have discovered a growing Arctic abiotic methane - and methane hydrate — charged
sediment drift on
oceanic crust in the deep Fram Strait
of the Arctic Ocean.
He uses
sediments, microfossils and geochemistry to study evidence
of past and present climate change in lake and
oceanic sediments, his CU biography states.