For more than 400 million years, mycorrhizal fungi and plants have formed partnerships that
are crucial to the emergence and functioning of global ecosystems. The importance of these …

Throughout Earth's history, CO2 is thought to have exerted a fundamental control on
environmental change. Here we review and revise CO2 reconstructions from boron isotopes …

Much of our understanding of Earth's past climate comes from the measurement of oxygen
and carbon isotope variations in deep-sea benthic foraminifera. Yet, long intervals in …

Abstract The Carbonate rock weathering Carbon Sink (CCS) and Silicate rock weathering
Carbon Sink (SCS) play a significant role in the carbon cycle and global climate change …

Concealed deep beneath the oceans is a carbon conveyor belt, propelled by plate tectonics.
Our understanding of its modern functioning is underpinned by direct observations, but its …

Scenarios to stabilize global climate and meet international climate agreements require
rapid reductions in human carbon dioxide (CO2) emissions, often augmented by substantial …

Abstract The 'COPSE'(Carbon, Oxygen, Phosphorus, Sulphur and Evolution)
biogeochemical model predicts the coupled histories and controls on atmospheric O 2, CO 2 …

Mammals have dominated Earth for approximately 55 Myr thanks to their adaptations and
resilience to warming and cooling during the Cenozoic. All life will eventually perish in a …

Over the past century a number of models have been developed to explain the vast
stratigraphic distribution of authigenic dolomite. These models include hydrogeological …

Although pH is a fundamental property of Earth's oceans, critical to our understanding of
seawater biogeochemistry, its long-timescale geologic history is poorly constrained. We …