Global Climate Change Digest: Main Page | Introduction | Archives | Calendar | Copy Policy | Abbreviations | Guide to Publishers

GCRIO Home ->arrow Library ->arrow Archives of the Global Climate Change Digest ->arrow August 1992 ->arrow PROFESSIONAL PUBLICATIONS... MARINE BIOGEOCHEMISTRY & FERTILIZATION Search

U.S. Global Change Research Information Office logo and link to home

Last Updated:
February 28, 2007

GCRIO Program Overview



Our extensive collection of documents.


Get Acrobat Reader

Privacy Policy

Global Climate Change DigestArchives of the
Global Climate Change Digest

A Guide to Information on Greenhouse Gases and Ozone Depletion
Published July 1988 through June 1999



Item #d92aug68

"Episodic Atmospheric Nitrogen Deposition to Oligotrophic Oceans," N.J.P. Owens (Marine Lab., Prospect Pl., The Hoe, Plymouth PL1 3DH, UK), J.N. Galloway, R.A. Duce, Nature, 357(6377), 397-399, June 4, 1992.

Reevaluates atmospheric N inputs using a nine-year record of N deposition, and shows that they can make important contributions to "new production" of phytoplankton during episodic events. The burning of fossil fuels could directly increase oceanic productivity through this mechanism.

Item #d92aug69

"Carbon Fluxes and Burial Rates over the Continental Slope and Rise off Central California with Implications for the Global Carbon Cycle," C.E. Reimers (Scripps Inst. Oceanog., La Jolla CA 92093), R.A. Jahnke, D.C. McCorkle, Global Biogeochem. Cycles, 6(2), 199 ff., June 1992.

Measurements of organic carbon degradation and CaCO3 dissolution were combined with organic-C and carbonate-C accumulation rates. Results suggest that modern sediments on the outer regions of continental margins are important sources of CO2 that is injected directly into ocean deep water, but do not indicate a significant anthropogenic enhancement of carbon export to continental slopes and rises.

Item #d92aug70

Three items from Nature, 356(6371), Apr. 23, 1992:

"Catalytic Conversions," J.R. Toggweiler (GFDL, Princeton Univ., POB 308, Princeton NJ 08542), 665-666.

Critically discusses the somewhat conflicting results of the next two papers in this issue of Nature and the following paper by Benner et al. in Science. They relate to the controversial findings of Sugimura and Suzuki (1988), who claimed to discover a new pool of dissolved organic carbon (DOC) based on a new extraction method, high-temperature catalytic oxidation (HTCO).

"Comparison of Two Methods for Measuring Dissolved Organic Carbon in Sea Water," H. Ogawa (Dept. Environ. Sci., Tokyo Univ. Agric. & Technol., 3-5-8 Saiwaicho, Fuchu-shi, Tokyo 183, Japan), N. Ogura, 696-698.

Compares determinations of DOC obtained by HTCO with conventional determination by wet chemical oxidation (WCO). The results are in fair agreement, with the HTCO results being considerably lower than reported previously.

"Dissolved Organic Carbon in the Atlantic, Southern and Pacific Oceans," J.H. Martin (Moss Landing Marine Labs., Moss Landing CA 95039), S.E. Fitzwater, 699-700.

Provides independent confirmation of the findings of Sugimura and Suzuki using the HTCO technique. Results imply that the carbon content of the oceans has previously been underestimated by 1012 tons, and that the new total represents one of the largest carbon reservoirs on Earth.

Item #d92aug71

"Bulk Chemical Characteristics of Dissolved Organic Matter in the Ocean," R. Benner (Marine Sci. Inst., Univ. Texas, Port Aransas TX 78373), J.D. Pakulski et al., Science, 255(5051), 1561-1564, Mar. 20, 1992.

Uses ultrafiltration to recover milligram amounts of >1000 daltons of DOM from three depths in the North Pacific Ocean. Polysaccharides appear to be more abundant and reactive components of sea water DOM than has been recognized.

Item #d92aug72

"Downward Transport and Fate of Organic Matter in the Ocean: Simulations with a General Circulation Model," R.G. Najjar (NCAR, POB 3000, Boulder CO 80307), J.L. Sarmiento, J.R. Toggweiler, Global Biogeochem. Cycles, 6(1), 45 ff., Mar. 1992.

A phosphorous-based model of nutrient cycling combined with a general circulation model is used to explore "nutrient trapping," a positive feedback whereby upwelling contributes to new production. Results support the HTCO results of Sugimura and Suzuki (1988) and suggest the existence of an as yet undiscovered pool of dissolved organic phosphorous in the ocean.

Item #d92aug73

"Nutrient Control of Phytoplankton Photosynthesis in the Western North Atlantic," T. Platt (Bedford Inst. Oceanog., Box 1006, Dartmouth, N.S. B2Y 4A2, Can.), S. Sathyendranath et al., Nature, 356(6366), 229-231, Mar. 19, 1992.

Results from several years of oceanographic cruises on the parameters of the photosynthesis-light curve for marine flora are interpreted as direct evidence for nutrient control of photosynthesis in the open ocean. Other significant implications for the ocean carbon cycle are discussed.

Item #d92aug74

"The BOFS 1990 Spring Bloom Experiment--Temporal Evolution and Spatial Variability of the Hydrographic Field," G. Savidge (Marine Biol. Sta., Queens Univ. Belfast, Portaferry BT22 1PF, Down, N. Ireland), D.R. Turner et al., Progr. Oceanog., 29(3), 235-281, 1992.

A lengthy review of the first major experiment of the U.K. Biogeochemical Ocean Flux Study (BOFS), intended to monitor and quantify the carbon flux changes associated with the evolution of the spring bloom in the northeast Atlantic. Mesoscale features were observed to have a major influence on the development of the bloom.

Item #d92aug75

"Photo-Reduction of Fe(III) by Dissolved Organic Substances and Existence of Fe(II) in Seawater during Spring Blooms," K. Kuma (Dept. Chem., Fisheries Faculty, Hokkaido Univ., Hakodate 041, Japan), S. Nakabayashi et al., Marine Chem., 37(1-2), 15-27, Mar. 1992.

Laboratory experiments showed that Fe (III) was readily reduced to Fe (II) in sunlight in the presence of hydroxycarboxylic acids, such as sugar acids. In the field, Fe (II) appeared in oxic surface sea water during spring blooms, possibly as a result of photoreduction of Fe (III) in the presence of hydroxycarboxylic acids released by phytoplankton.

Item #d92aug76

"Link between Iron and Sulfur Cycles Suggested by Detection of Fe(II) in Remote Marine Aerosols," G. Zhuang (Environ. Sci. Prog., Univ. Massachusetts, 100 Morrissey Blvd., Boston MA 02125), Z. Yi et al., Nature, 355(6360), 537-539, Feb. 6, 1992.

Fe (II) contributed about half of the total Fe in marine aerosol samples collected over the Pacific and at Barbados. In view of the marine biological production of DMS and the subsequent oxidation of reduced forms of atmospheric S, the Fe and S cycles in both the atmosphere and ocean may be closely coupled.

Item #d92aug77

"Quantitative Spatial Models of Atlantic Primary Productivity: An Application of Geomathematics," U.C. Herzfeld (Scripps Inst. Oceanog., La Jolla CA 92093), J. Geophys. Res., 97(C1), 717-732, Jan. 15, 1992.

The role of physical oceanographical, geochemical and sedimentological data in the problem of estimating ocean primary productivity is analyzed using geostatistical and algebraic multivariate spatial methods. Presents Atlantic Ocean case studies for phosphate distribution at the 100 m level, foraminifera abundance in sediments, and sea surface temperature.

Item #d92aug78

Special section on the WEC88 cruise to the equatorial Pacific, J. Geophys. Res., 97(C1), Jan. 15, 1992.

"Introduction to the WEC88 Cruise: An Investigation into Why the Equator Is Not Greener," R.T. Barber (Marine Lab., Duke Univ., Beaufort, N.C.), 609-610. The cruise focused on upwelling, turbulence, irradiance and nutrient supply, and how they affect photosynthesis, photoadaptation, nutrient uptake and the synthesis of new nitrogen- and carbon-containing biomass. By showing that physical conditions are not responsible for the persistence of unused nutrients in surface waters, the results emphasize the need to test the role of grazing and the iron hypothesis.

"Hydrographic Patterns and Vertical Mixing in the Equatorial Pacific along 150? W," M.-E. Carr (College Oceanog., Oregon State Univ., Corvallis OR 97331), N.S. Oakey et al., 611-626.

"Primary Production Estimates from Recordings of Solar Stimulated Fluorescence in the Equatorial Pacific at 150? W," P.M. Stegmann (Grad. Sch. Oceanog., Univ. Rhode Island, Narraganset RI 02882), M.R. Lewis et al., 627-638.

"Photosynthetic Characteristics and Estimated Growth Rates Indicate Grazing Is the Proximate Control of Primary Production in the Equatorial Pacific," J.J. Cullen (Dept. Oceanog., Dalhousie Univ., Halifax, N.S. B3H 4J1, Can.), M.R. Lewis et al., 639-654.

"Standing Stocks of Particulate Carbon and Nitrogen in the Equatorial Pacific at 150? W," R.W. Eppley (Marine Life Res. Group, Scripps Inst. Oceanog., La Jolla CA 92093), F.P. Cahvez, R.T. Barber, 655-661.

"Nitrate Utilization by Plankton in the Equatorial Pacific, March 1988, along 150? W," R.E. Eppley (addr. above), E.H. Renger, 663-668.

"Measurements of Nitrogen Productivity in the Equatorial Pacific," F.P. Wilkerson (Dept. Biol. Sci., Univ. Southern California, Los Angeles CA 90089), R.C. Dugdale, 669-679.

"Estimating New Production in the Equatorial Pacific Ocean at 150? W," R.C. Dugdale (Dept. Biol. Sci., Univ. Southern California, Los Angeles CA 90089), F.P. Wilkerson et al., 681-686.

Item #d92aug79

Two items from Science, 254(5036), Nov. 29, 1991:

"Age of Canada Basin Deep Waters: A Way to Estimate Primary Production for the Arctic Ocean," R.W. Macdonald (Inst. Ocean Sci., POB 6000, Sidney, B.C. V8L 4B2, Can.), E.C. Carmack, 1348-1350.

An empirical model of carbon flux and 14C-derived age of water as a function of depth was used to estimate the long-term rate of primary production, providing a baseline for understanding the role of the Arctic Ocean in global carbon cycling.

"Major Role of the Cyanobacterium Trichodesmium in Nutrient Cycling in the North Atlantic Ocean," E.J. Carpenter (Marine Sci. Res. Ctr., SUNY, Stony Brook NY 11794), K. Romans, 1356-1358.

Abundance measurements of this large phytoplankter plus a review of earlier observations indicate that it, rather than the picophytoplankton, is the most important primary producer in the tropical North Atlantic Ocean. This finding may help explain the disparity between various methods of measuring productivity in the oligotrophic ocean.

Item #d92aug80

"Seasonal and Depth-Related Changes in the Source of Sinking Particles in the North Atlantic," M.A. Altabet (Woods Hole Oceanog. Inst., Woods Hole MA 02543), W.G. Deuser et al., Nature, 354(6349), 136-139, Nov. 14, 1991.

Uses nitrogen isotope ratios to investigate the source and transformation of large, fast-sinking particles in the North Atlantic Ocean. The signal from near-surface seasonal changes propagates rapidly into the deep ocean. There may be another source of sinking particles other than recent surface production.

Item #d92aug81

"Occurrence of Small Colloids in Sea Water," M.L. Wells (Scripps Inst. Oceanog., La Jolla CA 92093), E.D. Goldberg, ibid., 353(6342), 342 ff., Sep. 26, 1991.

Measurements show that marine colloids <120 nm in size are at least three orders of magnitude more abundant than larger (submicrometer) particles, and their depth distribution differs markedly. Their existence may contribute to the discrepancy between standard and new high-temperature methods for measuring dissolved organic carbon.

Item #d92aug82

"Carbon Monoxide and Methane Distribution and Consumption in the Photic Zone of the Sargasso Sea," R.D. Jones (Dept. Biol. Sci., Florida Intl. Univ., Miami, Fla.), Deep Sea Res., Pt. A. Oceanog. Res. Papers (U.K.), 38(6A), 625-635, June 1991.

Distributions and microbial oxidation of CO and CH4 were examined on three cruises. Due to the long turnover times found for these trace gases, their oxidation by bacteria is unlikely to represent a significant link within the carbon cycle in these highly oligotrophic waters.

  • Guide to Publishers
  • Index of Abbreviations

  • Hosted by U.S. Global Change Research Information Office. Copyright by Center for Environmental Information, Inc. For more information contact U.S. Global Change Research Information Office, Suite 250, 1717 Pennsylvania Ave, NW, Washington, DC 20006. Tel: +1 202 223 6262. Fax: +1 202 223 3065. Email: Web: Webmaster:
    U.S. Climate Change Technology Program Intranet Logo and link to Home