Results 211 to 220 of about 41,861 (265)
Some of the next articles are maybe not open access.
The Nature of Marine Sediments
2007The discussion in this chapter will be restricted to surficial sediments (upper few meters) found on the continental shelf (beach to the continental shelf-slope break, approximately to 100–130 m water depth) and in other nearshore environments (lagoons, estuaries, and bays).
Darrell R. Jackson +1 more
openaire +1 more source
Deep Sea Research Part A. Oceanographic Research Papers, 1979
Abstract Interstitial methane profiles from six sediment cores taken on the slope and abyssal plain of the Gulf of Mexico can be explained by simple kinetic modeling. Methane is apparently produced at a constant rate and microbially consumed in the sulfate-reducing zone.
openaire +1 more source
Abstract Interstitial methane profiles from six sediment cores taken on the slope and abyssal plain of the Gulf of Mexico can be explained by simple kinetic modeling. Methane is apparently produced at a constant rate and microbially consumed in the sulfate-reducing zone.
openaire +1 more source
The Mineralogy of Marine Sediments
1989Those grains that were originally formed on the continents and have subsequently been transported into the ocean. River transport is the most important mechanism in which terrigenous minerals are passed to the ocean realm. Milliman & Meade (1983) estimate that about 12–13 × 109 tonnes of suspended sediment are supplied to the oceans by rivers annually ...
openaire +1 more source
New Microbial Biodiversity in Marine Sediments
Annual Review of Marine Science, 2021Xianzhe Gong +2 more
exaly
Gas in Marine Sediments—an introduction
Marine Geology, 1997vanWeering, TCE, Klaver, GT, Prins, RA
openaire +2 more sources