Organic carbon in marine sediments is a critical component of the global carbon cycle, and
its degradation influences a wide range of phenomena, including the magnitude of carbon …

Interest in extracting mineral resources from the seafloor through deep‐sea mining has
accelerated in the past decade, driven by consumer demand for various metals like zinc …

The efficiency of carbon sequestration by the biological pump could decline in the coming
decades because respiration tends to increase more with temperature than photosynthesis …

Uncertainties in projections of marine biogeochemistry from Earth system models (ESMs)
are associated to a large degree with the imperfect representation of the marine plankton …

In this contribution, we explore the idea that the Ca isotope proxy has utility as an indicator of
carbonate authigenesis (ie, post-depositional precipitation of CaCO 3 within the sedimentary …

We developed a coupling scheme for the Community Earth System Model version 1.2
(CESM1. 2) and the Model of Early Diagenesis in the Upper Sediment of Adjustable …

The coupled biogeochemical cycles of iron and sulphur are central to the long-term
biogeochemical evolution of Earth's oceans. For instance, before the development of a …

The isotopic composition of Si in biogenic silica (BSi), such as opal buried in the oceans'
sediments, has changed over time. Paleorecords suggest that the isotopic composition …

Extreme warming at the end-Permian induced profound changes in marine biogeochemical
cycling and animal habitability, leading to the largest extinction in Earth's history. However, a …

Programmed cell death may have important intra and inter-specifics effects in
phytoplanktonic populations, and consequently in the ecology of freshwater ecosystems …