TY - BOOK ID - 145951522 TI - Climate Change and Marine Geological Dynamics AU - Kontakiotis, George AU - Antonarakou, Assimina PY - 2021 PB - Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute DB - UniCat KW - Research & information: general KW - microfacies types KW - Pantokrator Limestones KW - Vigla Formation KW - Senonian calciturbidites KW - Eocene brecciated limestones KW - carbonate porosity KW - petroleum prospectivity KW - stratigraphic correlations KW - marine biogenic carbonates KW - depositional environment KW - paleoceanographic evolution KW - planktonic foraminifera KW - pteropods KW - stable isotopes KW - sea surface temperature (SST) KW - stratification KW - productivity KW - sapropel S1 KW - Aegean Sea KW - Late Quaternary KW - shell weight KW - climate variability KW - sea surface density KW - carbonate production KW - X-ray microscopy (μCT) KW - δ18O and Mg/Ca analyses KW - offshore groundwater exploration KW - coastal aquifers KW - salt-/fresh-water relationship KW - Mediterranean Sea KW - Attica-Greece KW - cleaning protocol KW - unconsolidated core sediments KW - climate reconstruction KW - synchrotron X-ray microtomography (SμCT) KW - foraminiferal-based proxies KW - BTEX natural attenuation KW - hydro-stratigraphy KW - multi-layered aquifer KW - Thriassion Plain KW - confined and unconfined aquifer KW - coastal aquifer KW - Gulf of Eleusis KW - ocean paleodensity KW - Atlantic Meridional Circulation (AMOC) KW - planktonic foraminiferal biogeography KW - surface sediments KW - morphometrics KW - shell size KW - environmental biomonitoring KW - ecological optimum conditions KW - primary productivity KW - depth habitat preference KW - cryptic speciation KW - central Mediterranean hydrodynamics KW - sea level fluctuations KW - soluble substances KW - coastal environment change KW - diatom KW - geochemical elements KW - microfacies types KW - Pantokrator Limestones KW - Vigla Formation KW - Senonian calciturbidites KW - Eocene brecciated limestones KW - carbonate porosity KW - petroleum prospectivity KW - stratigraphic correlations KW - marine biogenic carbonates KW - depositional environment KW - paleoceanographic evolution KW - planktonic foraminifera KW - pteropods KW - stable isotopes KW - sea surface temperature (SST) KW - stratification KW - productivity KW - sapropel S1 KW - Aegean Sea KW - Late Quaternary KW - shell weight KW - climate variability KW - sea surface density KW - carbonate production KW - X-ray microscopy (μCT) KW - δ18O and Mg/Ca analyses KW - offshore groundwater exploration KW - coastal aquifers KW - salt-/fresh-water relationship KW - Mediterranean Sea KW - Attica-Greece KW - cleaning protocol KW - unconsolidated core sediments KW - climate reconstruction KW - synchrotron X-ray microtomography (SμCT) KW - foraminiferal-based proxies KW - BTEX natural attenuation KW - hydro-stratigraphy KW - multi-layered aquifer KW - Thriassion Plain KW - confined and unconfined aquifer KW - coastal aquifer KW - Gulf of Eleusis KW - ocean paleodensity KW - Atlantic Meridional Circulation (AMOC) KW - planktonic foraminiferal biogeography KW - surface sediments KW - morphometrics KW - shell size KW - environmental biomonitoring KW - ecological optimum conditions KW - primary productivity KW - depth habitat preference KW - cryptic speciation KW - central Mediterranean hydrodynamics KW - sea level fluctuations KW - soluble substances KW - coastal environment change KW - diatom KW - geochemical elements UR - https://www.unicat.be/uniCat?func=search&query=sysid:145951522 AB - 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. ER -