Seasonal spillover and varve formation in the Santa Barbara Basin, California Public Deposited

http://ir.library.oregonstate.edu/concern/defaults/xk81jm76w

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  • A temporal record of oxygen and NO3- concentrations in the bottom water of the Santa Barbara Basin indicates that outside waters spill over into the basin seasonally. It is proposed that an annual bottom-water cycle leads ultimately to varve production. As evidence in support of a benthic mechanism for varve formation, we present results of surface sediment and pore-water analyses, from box-core collections during three seasons in 1988. The greater degree of bottom-water oxygen depletion that occurs regularly in late summer and fall was coincident with a smaller pool of pore-water Fe, penetration of ΣH2S up to the sediment-water interface, maximal numbers of benthic Foraminifera, and bacterial mat growth. The latter was indicated by increases in concentrations of extractable ATP, organic C, and total N in sediments from the depth intervals 0–0.25 and 0.25–0.5 cm. The greatest numbers of siliceous phytoplankton skeletons were found on the sea floor soon after the late spring, surface-water, Chl a maximum. This event coincides with additions of new and more-oxygenated seawater to the deep basin.
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  • Limnol. Oceanog. 35, 1577-1585
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  • description.provenance : Approved for entry into archive by Linda Lamb(llamb@coas.oregonstate.edu) on 2009-11-23T18:35:25Z (GMT) No. of bitstreams: 1 LimnolOceanograph 1990 35 1577-1585.pdf: 1882568 bytes, checksum: b07271e8d462c865a59dfe285e22a600 (MD5)
  • description.provenance : Made available in DSpace on 2009-11-23T18:35:25Z (GMT). No. of bitstreams: 1 LimnolOceanograph 1990 35 1577-1585.pdf: 1882568 bytes, checksum: b07271e8d462c865a59dfe285e22a600 (MD5) Previous issue date: 1990
  • description.provenance : Submitted by Linda Lamb (llamb@coas.oregonstate.edu) on 2009-11-23T18:18:43Z No. of bitstreams: 1 LimnolOceanograph 1990 35 1577-1585.pdf: 1882568 bytes, checksum: b07271e8d462c865a59dfe285e22a600 (MD5)
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  • 0024-3590

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