High-pressure low-temperature (HP–LT) metamorphic rocks provide invaluable constraints on the evolution of convergent zones. Based on a worldwide compilat...
High-pressure low-temperature (HP–LT) metamorphic rocks provide invaluable constraints on the evolution of convergent zones. Based on a worldwide compilat...
A series of M-b 3.8-5.5 induced seismic events in the midcontinent region, United States, resulted from injection of fluid either into a basal sedimentary ...
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Sporadic temporal and spatial increases in primary production, reflecting changes in the behavior and/or state of the ocean-atmosphere system, constitute a...
Applied organic geochemistry provides the information needed to make maps of the richness, type, and thermal maturity of a source rock. These maps are a ne...
The intensity, duration and frequency of coastal hypoxia (oxygen concentration <63 ??M) are increasing due to human alteration of coastal ecosystems and ch...
Presents a study which examined the chemostratigraphy of the Jurassic system. Factors which affected the development of organic-rich sediments; Controls o...
Current chemostratigraphical studies of the Jurassic System primarily involve the use of one sedimentary component (marine organic carbon), one divalent tr...
The analogy between desert oasis and deep-sea chemosynthetic community arose from the biomass contrast between vents and the relatively depauperate backgro...
A newly compiled global reef database indicates that the 5鈥 6 Myr long Frasnian (Late Devonian) metazoan reef episode had relatively low diversity compared...
Phosphorus (P) is a limiting nutrient for terrestrial biological productivity that commonly plays a key role in net carbon uptake in terrestrial ecosystems...
The diagenesis and preservation of organic matter in marine sediments has received considerable attention in the past several years. Studies have quantified rates of organic carbon oxidation in sediments and how these rates vary among se...