Climate Change and Marine Geological Dynamics

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...

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Առցանց հասանելիություն:ONIX_20220111_9783036516981_555
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collection Directory of Open Access Books
description 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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publisher MDPI - Multidisciplinary Digital Publishing Institute
publisherStr MDPI - Multidisciplinary Digital Publishing Institute
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spelling doab-20.500.12854ir-768202024-03-27T16:34:38Z Climate Change and Marine Geological Dynamics Kontakiotis, George Antonarakou, Assimina microfacies types Pantokrator Limestones Vigla Formation Senonian calciturbidites Eocene brecciated limestones carbonate porosity petroleum prospectivity stratigraphic correlations marine biogenic carbonates depositional environment paleoceanographic evolution planktonic foraminifera pteropods stable isotopes sea surface temperature (SST) stratification productivity sapropel S1 Aegean Sea Late Quaternary shell weight climate variability sea surface density carbonate production X-ray microscopy (μCT) δ18O and Mg/Ca analyses offshore groundwater exploration coastal aquifers salt-/fresh-water relationship Mediterranean Sea Attica-Greece cleaning protocol unconsolidated core sediments climate reconstruction synchrotron X-ray microtomography (SμCT) foraminiferal-based proxies BTEX natural attenuation hydro-stratigraphy multi-layered aquifer Thriassion Plain confined and unconfined aquifer coastal aquifer Gulf of Eleusis ocean paleodensity Atlantic Meridional Circulation (AMOC) planktonic foraminiferal biogeography surface sediments morphometrics shell size environmental biomonitoring ecological optimum conditions primary productivity depth habitat preference cryptic speciation central Mediterranean hydrodynamics sea level fluctuations soluble substances coastal environment change diatom geochemical elements n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general 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. 2022-01-11T13:43:11Z 2022-01-11T13:43:11Z 2021 book ONIX_20220111_9783036516981_555 9783036516981 9783036516974 https://directory.doabooks.org/handle/20.500.12854/76820 eng image/jpeg Attribution 4.0 International https://mdpi.com/books/pdfview/book/4269 https://mdpi.com/books/pdfview/book/4269 MDPI - Multidisciplinary Digital Publishing Institute 10.3390/books978-3-0365-1697-4 10.3390/books978-3-0365-1697-4 46cabcaa-dd94-4bfe-87b4-55023c1b36d0 9783036516981 9783036516974 183 Basel, Switzerland open access
spellingShingle microfacies types
Pantokrator Limestones
Vigla Formation
Senonian calciturbidites
Eocene brecciated limestones
carbonate porosity
petroleum prospectivity
stratigraphic correlations
marine biogenic carbonates
depositional environment
paleoceanographic evolution
planktonic foraminifera
pteropods
stable isotopes
sea surface temperature (SST)
stratification
productivity
sapropel S1
Aegean Sea
Late Quaternary
shell weight
climate variability
sea surface density
carbonate production
X-ray microscopy (μCT)
δ18O and Mg/Ca analyses
offshore groundwater exploration
coastal aquifers
salt-/fresh-water relationship
Mediterranean Sea
Attica-Greece
cleaning protocol
unconsolidated core sediments
climate reconstruction
synchrotron X-ray microtomography (SμCT)
foraminiferal-based proxies
BTEX natural attenuation
hydro-stratigraphy
multi-layered aquifer
Thriassion Plain
confined and unconfined aquifer
coastal aquifer
Gulf of Eleusis
ocean paleodensity
Atlantic Meridional Circulation (AMOC)
planktonic foraminiferal biogeography
surface sediments
morphometrics
shell size
environmental biomonitoring
ecological optimum conditions
primary productivity
depth habitat preference
cryptic speciation
central Mediterranean hydrodynamics
sea level fluctuations
soluble substances
coastal environment change
diatom
geochemical elements
n/a
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
Climate Change and Marine Geological Dynamics
title Climate Change and Marine Geological Dynamics
title_full Climate Change and Marine Geological Dynamics
title_fullStr Climate Change and Marine Geological Dynamics
title_full_unstemmed Climate Change and Marine Geological Dynamics
title_short Climate Change and Marine Geological Dynamics
title_sort climate change and marine geological dynamics
topic microfacies types
Pantokrator Limestones
Vigla Formation
Senonian calciturbidites
Eocene brecciated limestones
carbonate porosity
petroleum prospectivity
stratigraphic correlations
marine biogenic carbonates
depositional environment
paleoceanographic evolution
planktonic foraminifera
pteropods
stable isotopes
sea surface temperature (SST)
stratification
productivity
sapropel S1
Aegean Sea
Late Quaternary
shell weight
climate variability
sea surface density
carbonate production
X-ray microscopy (μCT)
δ18O and Mg/Ca analyses
offshore groundwater exploration
coastal aquifers
salt-/fresh-water relationship
Mediterranean Sea
Attica-Greece
cleaning protocol
unconsolidated core sediments
climate reconstruction
synchrotron X-ray microtomography (SμCT)
foraminiferal-based proxies
BTEX natural attenuation
hydro-stratigraphy
multi-layered aquifer
Thriassion Plain
confined and unconfined aquifer
coastal aquifer
Gulf of Eleusis
ocean paleodensity
Atlantic Meridional Circulation (AMOC)
planktonic foraminiferal biogeography
surface sediments
morphometrics
shell size
environmental biomonitoring
ecological optimum conditions
primary productivity
depth habitat preference
cryptic speciation
central Mediterranean hydrodynamics
sea level fluctuations
soluble substances
coastal environment change
diatom
geochemical elements
n/a
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
topic_facet microfacies types
Pantokrator Limestones
Vigla Formation
Senonian calciturbidites
Eocene brecciated limestones
carbonate porosity
petroleum prospectivity
stratigraphic correlations
marine biogenic carbonates
depositional environment
paleoceanographic evolution
planktonic foraminifera
pteropods
stable isotopes
sea surface temperature (SST)
stratification
productivity
sapropel S1
Aegean Sea
Late Quaternary
shell weight
climate variability
sea surface density
carbonate production
X-ray microscopy (μCT)
δ18O and Mg/Ca analyses
offshore groundwater exploration
coastal aquifers
salt-/fresh-water relationship
Mediterranean Sea
Attica-Greece
cleaning protocol
unconsolidated core sediments
climate reconstruction
synchrotron X-ray microtomography (SμCT)
foraminiferal-based proxies
BTEX natural attenuation
hydro-stratigraphy
multi-layered aquifer
Thriassion Plain
confined and unconfined aquifer
coastal aquifer
Gulf of Eleusis
ocean paleodensity
Atlantic Meridional Circulation (AMOC)
planktonic foraminiferal biogeography
surface sediments
morphometrics
shell size
environmental biomonitoring
ecological optimum conditions
primary productivity
depth habitat preference
cryptic speciation
central Mediterranean hydrodynamics
sea level fluctuations
soluble substances
coastal environment change
diatom
geochemical elements
n/a
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
url ONIX_20220111_9783036516981_555