Documenting the mass flux through convergent plate margins is important to the
understanding of petrogenesis in arc settings and to the origin of the continental crust, since …

Water‐rock interactions within the seafloor are responsible for significant energy and solute
fluxes between basaltic oceanic crust and the overlying ocean. Permeability is the primary …

This paper presents new major and trace-element data and Lu–Hf and Sm–Nd isotopic
compositions for representative suites of marine sediment samples from 14 drill sites …

Stable carbon and oxygen isotopes (δ18O and δ13C values) and trace elements have been
applied to the study of diagenesis of carbonate rocks for over 50 years. As valuable as these …

The discovery of metal-depositing hot springs on the sea floor, and especially their link to
chemosynthetic life, was among the most compelling and significant scientific advances of …

The Paleocene‐Eocene thermal maximum (PETM) is one of the best known examples of a
transient climate perturbation, associated with a brief, but intense, interval of global warming …

The Middle Eocene Climatic Optimum (MECO) is an enigmatic warming event that
represents an abrupt reversal in long‐term cooling through the Eocene. In order to further …

Abstract The Paleocene‐Eocene Thermal Maximum (PETM) has been associated with the
release of several thousands of petagrams of carbon (Pg C) as methane and/or carbon …

Ideas about key factors in the oceanic mass balance of dissolved, reactive phosphate have
changed substantially. I present an integrated overview of these here, with an emphasis on …

We have compiled new and published data on the magnetic properties of 245 serpentinized
abyssal peridotites from seven Deep Sea Drilling Project and Ocean Drilling Program sites …