The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil and experimental analyses show that different species of marine calcifying algae responded very differently to the environmental upheavals
A high-resolution analysis of sediments recovered at ODP Site 1209B (Shatsky Rise – NW Pacific Ocean...
Predicting the impact of ongoing anthropogenic CO2 emissions on calcifying marine organisms is compl...
Abstract. Late Paleocene and Early Eocene climates and ecosystems underwent significant change durin...
The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil a...
The Paleocene-Eocene Thermal Maximum (PETM, ~5 million years ago) was an interval of global warming ...
The fossil record reveals large changes in marine plankton ecosystems linked with both environmental...
The Paleocene and Eocene are characterized by strong greenhouse climates. Atmospheric CO2 concentrat...
The Paleocene-Eocene Thermal Maximum (PETM, 55 million years ago) was an interval of global warming ...
Late Paleocene and early Eocene hyperthermals are transient warming events associated with massive p...
During rapid global warming 56 million years ago, tropical sea surface temperatures exceeded 36°C an...
Current carbon dioxide emissions are an assumed threat to oceanic calcifying plankton (coccolithopho...
Biotic response of calcareous nannoplankton to abrupt warming across the Paleocene/Eocene boundary r...
This paper provides a synthesis of the long- and short-term response of various marine ecosystems (d...
Biodiversity is expected to change in response to future global warming. However, it is difficult to...
Abrupt global warming and profound perturbation of the carbon cycle during the Paleocene-Eocene Ther...
A high-resolution analysis of sediments recovered at ODP Site 1209B (Shatsky Rise – NW Pacific Ocean...
Predicting the impact of ongoing anthropogenic CO2 emissions on calcifying marine organisms is compl...
Abstract. Late Paleocene and Early Eocene climates and ecosystems underwent significant change durin...
The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil a...
The Paleocene-Eocene Thermal Maximum (PETM, ~5 million years ago) was an interval of global warming ...
The fossil record reveals large changes in marine plankton ecosystems linked with both environmental...
The Paleocene and Eocene are characterized by strong greenhouse climates. Atmospheric CO2 concentrat...
The Paleocene-Eocene Thermal Maximum (PETM, 55 million years ago) was an interval of global warming ...
Late Paleocene and early Eocene hyperthermals are transient warming events associated with massive p...
During rapid global warming 56 million years ago, tropical sea surface temperatures exceeded 36°C an...
Current carbon dioxide emissions are an assumed threat to oceanic calcifying plankton (coccolithopho...
Biotic response of calcareous nannoplankton to abrupt warming across the Paleocene/Eocene boundary r...
This paper provides a synthesis of the long- and short-term response of various marine ecosystems (d...
Biodiversity is expected to change in response to future global warming. However, it is difficult to...
Abrupt global warming and profound perturbation of the carbon cycle during the Paleocene-Eocene Ther...
A high-resolution analysis of sediments recovered at ODP Site 1209B (Shatsky Rise – NW Pacific Ocean...
Predicting the impact of ongoing anthropogenic CO2 emissions on calcifying marine organisms is compl...
Abstract. Late Paleocene and Early Eocene climates and ecosystems underwent significant change durin...
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