Anthropogenic activity has affected the world’s oceans in various ways, causing warming, acidification and deoxygenation. Mechanisms driving and maintaining the latter can be understood by studying similar changes that occurred in the Earth’s past. This palynological study of Mid-Cretaceous (~94Ma) sediments from northern Canada sheds light on the drivers of anoxia and its development at higher latitudes. Changes in the palynological assemblages indicate that increased density stratification, through enhanced freshwater input and precipitation, were presumably the most important drivers. Changes in sea-level may have enhanced or counteracted the effects of stratification
Previous isotopic investigations of Aptian/Albian oceanic anoxic event (OAE) 1b from the western Nor...
Well-preserved nannofossil and stable isotope records from the mid-Cretaceous of Ocean Drilling Proj...
The Cretaceous evolution of calcareous plankton is characterized by a complex history punctuated by ...
Oceanic oxygen concentrations vary widely in space and time. Since oxygen is essential for (most) li...
Oxygen is a key element for life on earth. Oxygen concentrations in the ocean vary greatly in space ...
The Cretaceous Period (145-66 Ma) was a time of elevated global temperatures superimposed on fluctua...
abstract: The rates of marine deoxygenation leading to Cretaceous Oceanic Anoxic Events are poorly r...
Organic carbon-rich sediments are globally developed in pelagic sedimentary sequences of Aptian-Albi...
Organic carbon-rich sediments are globally developed in pelagic sedimentary sequences of Aptian-Albi...
The Cretaceous was a time of greenhouse climates characterized by at least 15 ˚C warmer sea surface ...
Oceanic anoxic events (OAEs) record profound changes in the climatic and paleoceanographic state of ...
The sedimentary record of the Late Cretaceous North American Western Interior Seaway (WIS) is charac...
The mid-Cretaceous is thought to be a greenhouse world with significantly higher atmospheric pCO2 an...
The Late Cretaceous Oceanic Anoxic Event 2 (OAE2; ca. 94 Ma) was one of the largest global carbon cy...
[1] Mid-Cretaceous (Barremian-Turonian) plankton preserved in deep-sea marl, organic-rich shale, and...
Previous isotopic investigations of Aptian/Albian oceanic anoxic event (OAE) 1b from the western Nor...
Well-preserved nannofossil and stable isotope records from the mid-Cretaceous of Ocean Drilling Proj...
The Cretaceous evolution of calcareous plankton is characterized by a complex history punctuated by ...
Oceanic oxygen concentrations vary widely in space and time. Since oxygen is essential for (most) li...
Oxygen is a key element for life on earth. Oxygen concentrations in the ocean vary greatly in space ...
The Cretaceous Period (145-66 Ma) was a time of elevated global temperatures superimposed on fluctua...
abstract: The rates of marine deoxygenation leading to Cretaceous Oceanic Anoxic Events are poorly r...
Organic carbon-rich sediments are globally developed in pelagic sedimentary sequences of Aptian-Albi...
Organic carbon-rich sediments are globally developed in pelagic sedimentary sequences of Aptian-Albi...
The Cretaceous was a time of greenhouse climates characterized by at least 15 ˚C warmer sea surface ...
Oceanic anoxic events (OAEs) record profound changes in the climatic and paleoceanographic state of ...
The sedimentary record of the Late Cretaceous North American Western Interior Seaway (WIS) is charac...
The mid-Cretaceous is thought to be a greenhouse world with significantly higher atmospheric pCO2 an...
The Late Cretaceous Oceanic Anoxic Event 2 (OAE2; ca. 94 Ma) was one of the largest global carbon cy...
[1] Mid-Cretaceous (Barremian-Turonian) plankton preserved in deep-sea marl, organic-rich shale, and...
Previous isotopic investigations of Aptian/Albian oceanic anoxic event (OAE) 1b from the western Nor...
Well-preserved nannofossil and stable isotope records from the mid-Cretaceous of Ocean Drilling Proj...
The Cretaceous evolution of calcareous plankton is characterized by a complex history punctuated by ...