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Climate Change and Marine Geological Dynamics
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The tendency for climate to change has been one of the most surprising outcomes of the study of Earth's history. Marine geoscience can reveal valuable information about past environments, climates, and biota just before, during and after each climate perturbation. Particularly, certain intervals of geological records are windows to key episodes in the climate history of the Earth–life system. Ιn this regard, the detailed analyses of such time intervals are challenging and rewarding for environmental reconstruction and climate modelling, because they provide documentation and better understanding of a warmer-than-present world, and opportunities to test and refine the predictive ability of climate models. Marine geological dynamics such as sea-level changes, hydrographic parameters, water quality, sedimentary cyclicity, and (paleo)climate are strongly related through a direct exchange between the oceanographic and atmospheric systems. The increasing attention paid to this wide topic is also motivated by the interplay of these processes across a variety of settings (coastal to open marine) and timescales (early Cenozoic to modern). In order to realize the full predictive value of these warm (fresh)/cold (salty) intervals in Earth's history, it is important to have reliable tools (e.g., integrated geochemical, paleontological and/or paleoceanographic proxies) through the application of multiple, independent, and novel techniques (e.g., TEX86, UK’37, Mg/Ca, Na/Ca, Δ47, and μCT) for providing reliable hydroclimate reconstructions at both local and global scales.
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Keywords
- Aegean Sea
- Atlantic Meridional Circulation (AMOC)
- Attica-Greece
- BTEX natural attenuation
- carbonate porosity
- carbonate production
- central Mediterranean hydrodynamics
- cleaning protocol
- climate reconstruction
- climate variability
- coastal aquifer
- coastal aquifers
- coastal environment change
- confined and unconfined aquifer
- cryptic speciation
- depositional environment
- depth habitat preference
- diatom
- ecological optimum conditions
- environmental biomonitoring
- Eocene brecciated limestones
- foraminiferal-based proxies
- geochemical elements
- Gulf of Eleusis
- hydro-stratigraphy
- Late Quaternary
- marine biogenic carbonates
- Mediterranean Sea
- microfacies types
- morphometrics
- multi-layered aquifer
- n/a
- ocean paleodensity
- offshore groundwater exploration
- paleoceanographic evolution
- Pantokrator Limestones
- petroleum prospectivity
- Planktonic Foraminifera
- planktonic foraminiferal biogeography
- primary productivity
- productivity
- pteropods
- Reference, information & interdisciplinary subjects
- Research & information: general
- salt-/fresh-water relationship
- sapropel S1
- sea level fluctuations
- sea surface density
- sea surface temperature (SST)
- Senonian calciturbidites
- shell size
- shell weight
- soluble substances
- Stable isotopes
- stratification
- stratigraphic correlations
- surface sediments
- synchrotron X-ray microtomography (SμCT)
- thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
- Thriassion Plain
- unconsolidated core sediments
- Vigla Formation
- X-ray microscopy (μCT)
- δ18O and Mg/Ca analyses
Links
DOI: 10.3390/books978-3-0365-1697-4Editions