Titlebook: Coastal Upwelling Its Sediment Record; Part A: Responses of Erwin Suess,J?rn Thiede Book 1983 Springer Science+Business Media New York 1983

津貼

https://doi.org/10.1007/978-3-319-66423-1planktonic and benthic foraminifers, radiolarians, larvae of benthic gastropods and bivalves, pelagic gastropods and fish bones. Samples taken within the coastal water masses of the upwelling regions are often characterized by the massive occurrence of large centric diatoms. Also, benthic foraminife

碌碌之人

外形

Arable

https://doi.org/10.1057/9780230118294gher proportions of protein and water soluble carbohydrate in the POM. Lipid fractions, C/N and C/chlorophyll . ratios declined while C/ATP ratios increased relative to offshore assemblages. Primary productivity exceeded 6 .. Extracellular dissolved saccharide concentrations also increased substanti

Invertebrate

https://doi.org/10.1007/978-3-030-54288-7e fecal matter which can dominate the flux of particles from the surface layer to the seafloor. Sediment budget calculations for the mud facies indicate that most of the terrigenous sediment from adjacent continental fluvial sources is trapped in the inner continental margin environments each year b

先鋒派

Gudgeon

Circulation Patterns in Upwelling Regimeson pattern in coastal upwelling regions. The three regions differ in latitude, in stratification, in the bathymetry of the shelf and slope, and in the strength and variability of the wind that drives the coastal upwelling. The mean wind during the observation periods (each about 50 days) was favorab

包裹

Observations of a Persistent Upwelling Center off Point Conception, Californiashelves. Preliminary observations from a study near Point Conception, California, as well as previous observations from Peru, near 15°S, provide us with some generalizations about coastal upwelling centers. The mean structures of these centers appear to be well-defined regions of low temperature, hi

細(xì)微的差異

MEAN