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- Geological Society of London Scientific Statement: what the geological record tells us about our present and future climate
- Global silicate weathering flux overestimated because of sediment-water cation exchange
- Emergence of the Southeast Asian islands as a driver for Neogene cooling
- A high-resolution summary of Cambrian to Early Triassic marine invertebrate biodiversity
- A Novel Hypothesis for the Role of Photosynthetic Physiology in Shaping Macroevolutionary Patterns
- Modeling Dragons: Using linked mechanistic physiological and microclimate models to explore environmental, physiological, and morphological constraints on the early evolution of dinosaurs
- The contribution to exogenic CO2 by contact metamorphism at continental arcs: A coupled model of fluid flux and metamorphic decarbonation
- Biologically mediated weathering in modern cryptogamic ground covers and the early Paleozoic fossil record
- Arc-continent collisions in the tropics set Earths climate state
- Concurrent origins of the genetic code and the homochirality of life, and the origin and evolution of biodiversity. Part II: Technical appendix
- The silicate weathering feedback in the context of ophiolite emplacement: Insights from an inverse model of global weathering proxies
- Modeling the consequences of land plant evolution on silicate weathering
- Model based Paleozoic atmospheric oxygen estimates: a revisit to GEOCARBSULF
- Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2
- The timescale of early land plant evolution
- Effect of paleoseawater composition on hydrothermal exchange in midocean ridges
- Marine life in a greenhouse world: cephalopod biodiversity and biogeography during the early Late Cretaceous
- A model for the decrease in amplitude of carbon isotope excursions across the Phanerozoic
- CO2 diffusion into pore spaces limits weathering rate of an experimental basalt landscape
- Mineral weathering and soil development in the earliest land plant ecosystems
- Low-latitude arc-continent collision as a driver for global cooling
- Continental arc volcanism as the principal driver of icehouse-greenhouse variability
- Eocene atmospheric CO2 from the nahcolite proxy
- A 30 Myr record of Late Triassic atmospheric pCO2 variation reflects a fundamental control of the carbon cycle by changes in continental weathering
- Error analysis of CO2 and O2 estimates from the long-term geochemical model GEOCARBSULF
- The Origin and Early Evolution of Roots
- Carbon isotopic evidence for organic matter oxidation in soils of the Old Red Sandstone (Silurian to Devonian, South Wales, UK)
- ASSESSMENT OF PEDOGENIC GIBBSITE AS A PALEO-PCO2 PROXY USING A MODERN ULTISOL
- Hydrologic Regulation of Chemical Weathering and the Geologic Carbon Cycle
- Seafloor spreading evolution in response to continental growth
- Coral reefs in the Anthropocene: persistence or the end of the line?
- 40Ar/39Ar age constraints on the Haifanggou and Lanqi formations: When did the first flowers bloom?
- Dynamic model constraints on oxygen-17 depletion in atmospheric O2 after a snowball Earth
- Cenozoic boron isotope variations in benthic foraminifers
- Section 4. Deep Time: Observational Evidence from the Sedimentary Rock Record
- Section 3. Introduction to the Geochemical Evolution of the Earth's Ecosphere
- Section 6. Deep Time: Modelling of Atmospheric CO2 and the Marine CO2-Carbonic Acid-Carbonate System
- Continental arc-island arc fluctuations, growth of crustal carbonates, and long-term climate change
- Lipid biomarkers record fundamental changes in the microbial community structure of tropical seas during the Late Ordovician Hirnantian glaciation
- The Chemistry of Carbon in Aqueous Fluids at Crustal and Upper-Mantle Conditions: Experimental and Theoretical Constraints
- From black mud to earth system science: A scientific autobiography
- Sequence development influenced by intermittent cooling events in the Cretaceous Aptian greenhouse, Adriatic platform, Croatia
- Hornwort pyrenoids, carbon-concentrating structures, evolved and were lost at least five times during the last 100 million years
- Biodiversity tracks temperature over time
- Estimating soil pCO2 using paleosol carbonates: implications for the relationship between primary productivity and faunal richness in ancient terrestrial ecosystems
- Leaf fossil record suggests limited influence of atmospheric CO2 on terrestrial productivity prior to angiosperm evolution
- Dynamic Causes of the Relation Between Area and Age of the Ocean Floor
- Eocene-Early Miocene paleotopography of the Sierra Nevada-Great Basin-Nevadaplano based on widespread ash-flow tuffs and paleovalleys
- REEF RECOVERY FOLLOWING THE FRASNIAN-FAMENNIAN (LATE DEVONIAN) MASS EXTINCTION: EVIDENCE FROM THE DUGWAY RANGE, WEST-CENTRAL UTAH
- A Simple Type of Wood in Two Early Devonian Plants
- Sea-Level Control on Source-Rock Development: Perspectives from the Holocene Black Sea, the Mid-Cretaceous Western Interior Basin of North America, and the Late Devonian Appalachian Basin
- Stratigraphic Control on Source-Rock Distribution: First and Second Order Scale
- The Deposition of Organic-Carbon-Rich Sediments: Models, Mechanisms, and Consequences-Introduction
- Controls on Organic Accumulation in Upper Jurassic Shales of Northwestern Europe as Inferred from Trace-Metal Geochemistry
- Fluvial Facies Models: Recent Developments
- Modeling the evolutionary rise of ectomycorrhiza on sub-surface weathering environments and the geochemical carbon cycle
- Towards a quantitative understanding of the late Neoproterozoic carbon cycle
- Atmospheric PCO2 Perturbations Associated with the Central Atlantic Magmatic Province
- Escargots through time: an energetic comparison of marine gastropod assemblages before and after the Mesozoic Marine Revolution
- Geologic constraints on the glacial amplification of Phanerozoic climate sensitivity
- Declining atmospheric CO2 during the late Middle Eocene climate transition
- Comparing early to middle Miocene terrestrial climate simulations with geological data
- THE EFFECT OF LEAF ORIENTATION TO SUNLIGHT ON STOMATAL PARAMETERS OF QUERCUS RUBRA AROUND THE BELGRADE LAKES, CENTRAL MAINE
- Hydrothermal dolomite in the Timiskaming outlier, central Canadian Shield: Proxy for Late Ordovician tectonic activity
- ENVIRONMENTAL AND ECOLOGICAL VARIABILITY OF MIDDLE DEVONIAN (GIVETIAN) FORESTS IN APPALACHIAN BASIN PALEOSOLS, NEW YORK, UNITED STATES
- Influences of alkalinity and pCO2 on CaCO3 nucleation from estimated Cretaceous composition seawater representative of "calcite seas"
- The effects of terrestrialization on marine ecosystems: the fall of CO2
- Controls on carbonate skeletal mineralogy: Global CO2 evolution and mass extinctions
- An atmospheric stimulus for cyanobacterial-bioinduced calcification ca. 350 million years ago?
- Is mid-late Paleozoic ocean-water chemistry coupled with epeiric seawater isotope records?
- Paradox of late Paleozoic glacioeustasy
- Methane and the CH4 related greenhouse effect over the past 400 million years
- Early Palaeozoic cooling events: peri-Gondwana and beyond
- Eve of biomineralization: Controls on skeletal mineralogy
- Paleogene paleosols and changes in pedogenesis during the initial Eocene thermal maximum: Big Bend National Park, Texas, USA
- Limits for Combustion in Low O2 Redefine Paleoatmospheric Predictions for the Mesozoic
- Trees and late Palaeozoic CO2 and O2
- Chemostatic modes of the ocean-atmosphere-sediment system through Phanerozoic time
- Weathering of soil minerals by angiosperm and gymnosperm trees
- The feedback between climate and weathering
- The Oxygen Cycle of the Terrestrial Planets: Insights into the Processing and History of Oxygen in Surface Environments
- Coral Reefs Under Rapid Climate Change and Ocean Acidification
- Paleoelevation Reconstruction using Pedogenic Carbonates
- Paleoenvironmental and Carbon-Oxygen Isotope Record of Middle Cambrian Carbonates (La Laja Formation) in the Argentine Precordillera
- Mesoproterozoic carbon dioxide levels inferred from calcified cyanobacteria
- Cybertectonic Earth and Gaia's weak hand: sedimentary geology, sediment cycling and the Earth system
- General circulation model simulation of the {delta}18O content of continental precipitation in the middle Cretaceous: A model-proxy comparison
- CO2-Forced Climate and Vegetation Instability During Late Paleozoic Deglaciation
- A Late Ordovician ice sheet in South America: Evidence from the Cancaniri tillites, southern Bolivia
- Faster seafloor spreading and lithosphere production during the mid-Cenozoic
- OXYGEN ISOTOPIC COMPOSITION OF BIOGENIC PHOSPHATE AND THE TEMPERATURE OF EARLY ORDOVICIAN SEAWATER
- The Phanerozoic Carbon Cycle: CO2 and O2 by Robert A. Berner