Ocean acidification may have severe consequences for marine ecosystems; however,
assessing its future impact is difficult because laboratory experiments and field observations …

The Cretaceous was one of the most remarkable periods in geological history, with a
“greenhouse” climate and several important geological events. Reconstructions of …

The limits for stomatal conductance are set by stomatal size (SS) and density (SD). An
inverse relationship between SS and SD has been observed in fossil and living plants. This …

We estimate tropical Atlantic upper ocean temperatures using oxygen isotope and Mg/Ca
ratios in well‐preserved planktonic foraminifera extracted from Albian through Santonian …

In recent years it has become apparent that the “cool tropic paradox” of Paleogene and
Cretaceous “greenhouse” climates arises because of the diagenetic alteration of tropical …

Although progress has been made in recent years in reconstructing the environmental
conditions at the Triassic/Jurassic Boundary (TJB), published records of atmospheric CO2 …

A comprehensive compilation of literature on global Cretaceous charcoal occurrences
shows that from the Valanginian on throughout the Cretaceous, terrestrial sedimentary …

Although some organisms exercise considerable control over their biomineralization,
seawater chemistry has affected skeletal secretion by many taxa. Secular changes in the …

Oceanic anoxic events (OAEs) are large-scale events of oxygen depletion in the deep ocean
that happened during pre-Cenozoic periods of extreme warmth. Here, to assess the role of …

Plant stomata display a wide range of short-term behavioural and long-term morphological
responses to atmospheric carbon dioxide concentration ([CO 2]). The diversity of responses …