Turnitin
降AI改写
早检测系统
早降重系统
Turnitin-UK版
万方检测-期刊版
维普编辑部版
Grammarly检测
Paperpass检测
checkpass检测
PaperYY检测
[HTML][HTML] Quaternary time scales for the Pontocaspian domain: Interbasinal connectivity and faunal evolution
Abstract The Pontocaspian (Black Sea-Caspian Sea) region has a very dynamic history of
basin development and biotic evolution. The region is the remnant of a once vast Paratethys …
basin development and biotic evolution. The region is the remnant of a once vast Paratethys …
Paratethys response to the Messinian salinity crisis
Abstract The Black Sea and Caspian Sea are the present-day remnants of a much larger
epicontinental sea on the Eurasian continental interior, the Paratethys. During the late …
epicontinental sea on the Eurasian continental interior, the Paratethys. During the late …
Middle Miocene paleoenvironmental crises in Central Eurasia caused by changes in marine gateway configuration
Marine gateways prove to be important factors for changes in the ecology and biochemistry
of marginal seas. Changes in gateway configuration played a dominant role in the Middle …
of marginal seas. Changes in gateway configuration played a dominant role in the Middle …
The geochemical riddle of “low-salinity gypsum” deposits
Gypsum makes up about one fifth of giant salt deposits formed by evaporation of seawater
throughout Earth's history. Although thermodynamic calculations and precipitation …
throughout Earth's history. Although thermodynamic calculations and precipitation …
Tectonics, base‐level fluctuations, and climate impact on the Eocene to present‐day erosional pattern of the Arabia‐Eurasia collision zone (NNW Iranian plateau and …
Abstract The NNW Iranian Plateau and west Alborz within the Arabia‐Eurasia collision zone
are characterized by three main tectono‐stratigraphic zones, crosscut by the Qezel‐Owzan …
are characterized by three main tectono‐stratigraphic zones, crosscut by the Qezel‐Owzan …
Flooding of the Caspian Sea at the intensification of Northern Hemisphere Glaciations
The semi-isolated epicontinental Paratethys Sea in the Eurasian continental interior was
highly sensitive to changes in basin connectivity and hydrological budget. The Caspian Sea …
highly sensitive to changes in basin connectivity and hydrological budget. The Caspian Sea …
[HTML][HTML] From Khersonian drying to Pontian “flooding”: late Miocene stratigraphy and palaeoenvironmental evolution of the Dacian Basin (Eastern Paratethys)
In the late Miocene, a large inland sea known as the Eastern Paratethys stretched out across
the present-day Black Sea–Caspian Sea region. The basin was mostly endorheic and its …
the present-day Black Sea–Caspian Sea region. The basin was mostly endorheic and its …
Quantifying the Mediterranean freshwater budget throughout the late Miocene: New implications for sapropel formation and the Messinian Salinity Crisis
The cyclic sedimentary record of the late Miocene Mediterranean shows a clear transition
from open marine to restricted conditions and finally to evaporitic environments associated …
from open marine to restricted conditions and finally to evaporitic environments associated …
The sensitivity of middle Miocene paleoenvironments to changing marine gateways in Central Europe
Abstract During the middle Miocene (15–12 Ma), the paleoenvironmental conditions in the
Paratethys Sea of Central Europe changed from normal marine to hypersaline and from …
Paratethys Sea of Central Europe changed from normal marine to hypersaline and from …
Messinian salinity crisis record under strong freshwater input in marginal, intermediate, and deep environments: The case of the North Aegean
In the present study, we investigate the Mediterranean–Paratethys connection during the
late Miocene in Strymon Basin (North Aegean, northeastern Mediterranean) and compare …
late Miocene in Strymon Basin (North Aegean, northeastern Mediterranean) and compare …