Cultivation of marine diatoms in the laboratory is under constant light condition, but the light environment in the field is not constant but mainly fluctuating, which leads to significant differences between the growth in indoor culture and that ...
10 14, 2022
The Eocene was a critical period in Earth's climate history that encompassed profound climatic and oceanographic reorganization from the greenhouse conditions of the early Eocene to the icehouse state of the early Oligocene. This interval was also...
10 13, 2022
Zero-valent sulfur (ZVS) is an important intermediate in the biogeochemical sulfur cycle, accumulated at sediment surfaces under the sea floor (including in cold seeps and hydrothermal vents). In previous studies, production of ZVS as the intermed...
10 11, 2022
Whether or not some form of plate tectonics operated during the Archaean eon, what tectonic regime may have preceded it, and how Earth transitioned into the modern plate tectonic regime, are fundamental questions that pertain to the development an...
09 30, 2022
Organic matter (OM) is a critical factor which regulates nitrogen loss pathways of denitrification and anammox for microbes in marine ecosystems. However, only a little attention has been paid to contrasting studies on denitrification and anammox ...
09 29, 2022
The westerly wind is an important part of the global climate system, driving the mid-latitude surface currents, regulating the exchange of heat, water vapor, and carbon between the ocean and the atmosphere, and having an important impact on region...
09 27, 2022
