International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass extinction crisis during the Phanerozoic. Caused by the volcanism of Deccan trapps and/or the impact of a meteorite, this mass extinction had a disastrous impact on calcareous nannofossils diversity leading to the most important turnover in their evolutionary history. The K/Pg mass extinction led also to an important change in the pelagic carbonate production and accumulation which has deeply perturbed the carbonate system. In this study, we aim to quantify nannofossil carbonate accumulation rates before and after the K/Pg boundary to discuss i) the impact of the volcanism on calcareous nannofossil size and carbonate production; ii) the impact o...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
The global extinctions linked to the Cretaceous-Tertiary (K-T) boundary severely affected marine pel...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
International audienceCalcareous nannoplankton is the main pelagic carbonate producer representing h...
The global extinctions linked to the Cretaceous-Tertiary (K-T) boundary severely affected marine pel...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...
International audienceCarbonate accumulation in the deep-sea is largely sustained by pelagic carbona...