Reconstructions of past sea surface temperatures (SSTs) are essential for understanding long-term climate variability, yet different proxy methods can…

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Abstract. The Maastrichtian (~72–66 Ma), the final stage of the Cretaceous, experienced long-term cooling with high atmospheric CO₂ and weak latitudinal temperature gradients. Tectonic movements and v...

Nuage - le Nuage de l'OSU Pytheas

Abstract. Constraining the thermodynamic conditions within an impact structure during and after hypervelocity impacts is extremely challenging due to the transi

Outside the comfort zone: physiological responses of marine calcifiers to extreme environmental conditions.