Micro- to Fine-Scale Chemical Gradients and Layers in Stratified Coastal Waters

[1]  H. Jannasch,et al.  Analytical Chemistry in Oceanography , 1992 .

[2]  L. Brand.  Minimum iron requirements of marine phytoplankton and the implications for the biogeochemical control of new production , 1991 .

[3]  P. Liss,et al.  The Role of Episodic Atmospheric Nutrient Inputs in the Chemical and Biological Dynamics of Oceanic Ecosystems , 1991 .

[4]  N. M. Price,et al.  Iron chemistry in seawater and its relationship to phytoplankton: a workshop report , 1995 .

[5]  Investigation of Small-Scale Vertical Mixing in Relation to the Temperature Structure in Stably Stratified Waters , 1975 .

[6]  G. Gill,et al.  The geochemistry of iron in puget sound , 1978 .

[7]  Casey C. Moore,et al.  Preliminary results from an in-situ spectral absorption meter , 1992, Optics & Photonics.

[8]  A. C. Redfield.  The processes determining the concentration of oxygen, phosphate and other organic derivatives within the depths of the Atlantic Ocean , 1942 .

[9]  Craig D. Taylor,et al.  Automated instrumentation for time-series measurement of primary production and nutrient status in production platform-accessible environments , 1993 .

[10]  S. Wofsy,et al.  Nitrogen metabolism of the eutrophic Delaware River ecosystem1 , 1986 .

[11]  W. Sunda,et al.  Iron uptake and growth limitation in oceanic and coastal phytoplankton , 1995 .

[12]  Charles S. Cox,et al.  Oceanic fine structure , 1972 .

[13]  Kenneth S. Johnson,et al.  A submersible flow analysis system , 1986 .

[14]  K. Johnson,et al.  Continuous determination of nitrate concentrations in situ , 1989 .