Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …

Soils comprise the largest terrestrial carbon (C) pool, containing both organic and inorganic
C. Soil inorganic carbon (SIC) was frequently disregarded because (1) it is partly heritage …

Enhanced silicate rock weathering (ERW), deployable with croplands, has potential use for
atmospheric carbon dioxide (CO2) removal (CDR), which is now necessary to mitigate …

Achieving national targets for net-zero carbon emissions will require atmospheric carbon
dioxide removal strategies compatible with rising agricultural production. One possible …

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

The nine editions of Stable Isotope Geochemistry have appeared over a time span of nearly
50 years. The first edition (1973) appeared as a slim book of 135 pages. Due to the rapid …

The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …

It has been 10 years since publication of the first edition ofSoils of the Past. In that time the
subject of paleopedology hasgrown rapidly, and established itself within the mainstream …

Paleosols (fossil soils) are preserved throughout the geologic record in depositional settings
ranging from alluvial systems to between basalt flows. Until recently, paleosols were studied …

The objectives of this synthesis are (1) to review the factors that influence the ecological,
geographical, and palaeoecological distributions of plants possessing C 4 photosynthesis …