Enigmatic relationship between chlorophyll a concentrations and photosynthetic rates at Station ALOHA.

An ordinary least squares (OLS) analysis of the relationship between chlorophyll a (chl a) concentrations and photosynthetic rates at depths of 5 and 25 m at Station ALOHA produced a slope that was only 28% of the mean productivity index at those depths and an intercept at zero chl a that equaled 70% of the mean photosynthetic rate. OLS regression lines are known to produce a slope and intercept that are biased estimates of the true slope and intercept when the explanatory variable, X, is uncontrolled, but in this case the measurement errors and natural variability of the chl a concentrations were much too small to explain the apparent bias. The bias was traceable to the fact that the photosynthetic rates were determined by more than one explanatory variable, a source of variability that is typically overlooked in discussions of OLS bias. Modeling the photosynthetic rates as a function of the product of chl a and surface irradiance produced a much more accurate and realistic description of the data, but the OLS continued to be biased, presumably because the photosynthetic rates were functions of factors in addition to chl a and surface irradiance (e.g., temperature, macronutrients, trace metals, and vitamins). The results underscore the need to recognize that the absence of bias in an OLS when X is not controlled implies that all scatter in the data about the OLS is due to errors in the dependent variable, an unlikely scenario. In most cases, resolution of the bias problem will require identification of the explanatory variables in addition to X that determine the dependent variable.

Prominent human health impacts from several marine microbes: history, ecology, and public health implications.

This paper overviews several examples of important public health impacts by marine microbes and directs readers to the extensive literature germane to these maladies. These examples include three types of dinoflagellates (Gambierdiscus spp., Karenia brevis, and Alexandrium fundyense), BMAA-producing cyanobacteria, and infectious microbes. The dinoflagellates are responsible for ciguatera fish poisoning, neurotoxic shellfish poisoning, and paralytic shellfish poisoning, respectively, that have plagued coastal populations over time. Research interest on the potential for marine cyanobacteria to contribute BMAA into human food supplies has been derived by BMAA's discovery in cycad seeds and subsequent implication as the putative cause of amyotrophic lateral sclerosis/parkinsonism dementia complex among the Chamorro people of Guam. Recent UPLC/MS analyses indicate that recent reports that BMAA is prolifically distributed among marine cyanobacteria at high concentrations may be due to analyte misidentification in the analytical protocols being applied for BMAA. Common infectious microbes (including enterovirus, norovirus, Salmonella, Campylobacter, Shigella, Staphylococcus aureus, Cryptosporidium, and Giardia) cause gastrointestinal and skin-related illness. These microbes can be introduced from external human and animal sources, or they can be indigenous to the marine environment.

Phaeothamniophyceae Classis Nova: A New Lineage of Chromophytes Based upon Photosynthetic Pigments, rbcL Sequence Analysis and Ultrastructure.

A new algal class, the Phaeothamniophyceae classis nova, is established from genera formerly classified in the Chrysophyceae (e.g., Chrysapion, Chrysoclonium, Chrysodictyon, Phaeobotrys, Phaeogloea, Phaeoschizochlamys, Phaeothamnion, Selenophaea, Sphaeridiothrix, Stichogloea, Tetrachrysis, Tetrapion and Tetrasporopsis) as well as one genus previously assigned to the Xanthophyceae (Pleurochloridella). HPLC analysis revealed the presence of fucoxanthin, diadinoxanthin, diatoxanthin, ß-carotene and heteroxanthin, in addition to chlorophylls a and c, in four genera (Phaeoschizochlamys, Phaeothamnion, Stichogloea, Pleurochloridella). The combination of fucoxanthin and heteroxanthin is known only for these organisms. The rbcL sequences of the same four genera, along with representatives of other chromophyte classes, were analyzed phylogenetically and provided independent support for recognition of the Phaeothamniophyceae as a distinct taxon. These data indicate that the Phaeothamniophyceae are more closely related to the classes Xanthophyceae and Phaeophyceae than to the Chrysophyceae. Electron microscopy revealed that Phaeoschizochlamys, Phaeothamnion and Stichogloea possess electron opaque vesicles at the cell periphery, have a cell wall that often appears laminate, form new daughter cell walls via eleutheroschisis, and have plastids with girdle lamellae and a ring-shaped genophore. The flagellar apparatus of Phaeothamnion zoospores (described in a previous study) is chosen as representative of the new class. The flagella are inserted laterally, basal bodies form an angle of ca. 145° or more, a multi-gyred flagellar transitional helix is present and tripartite flagellar hairs lack lateral filaments. Genera placed in the Phaeothamniophyceae are assigned to the orders Phaeothamniales and Pleurochloridellales, each with a single family.

Consistent fractionation of 13C in nature and in the laboratory: growth-rate effects in some haptophyte algae.

The carbon isotopic fractionation accompanying formation of biomass by alkenone-producing algae in natural marine environments varies systematically with the concentration of dissolved phosphate. Specifically, if the fractionation is expressed by epsilon p approximately delta e - delta p, where delta e and delta p are the delta 13C values for dissolved CO2 and for algal biomass (determined by isotopic analysis of C37 alkadienones), respectively, and if Ce is the concentration of dissolved CO2, micromole kg-1, then b = 38 + 160*[PO4], where [PO4] is the concentration of dissolved phosphate, microM, and b = (25 - epsilon p)Ce. The correlation found between b and [PO4] is due to effects linking nutrient levels to growth rates and cellular carbon budgets for alkenone-containing algae, most likely by trace-metal limitations on algal growth. The relationship reported here is characteristic of 39 samples (r2 = 0.95) from the Santa Monica Basin (six different times during the annual cycle), the equatorial Pacific (boreal spring and fall cruises as well as during an iron-enrichment experiment), and the Peru upwelling zone. Points representative of samples from the Sargasso Sea ([PO4] < or = 0.1 microM) fall above the b = f[PO4] line. Analysis of correlations expected between mu (growth rate), epsilon p, and Ce shows that, for our entire data set, most variations in epsilon p result from variations in mu rather than Ce. Accordingly, before concentrations of dissolved CO2 can be estimated from isotopic fractionations, some means of accounting for variations in growth rate must be found, perhaps by drawing on relationships between [PO4] and Cd/Ca ratios in shells of planktonic foraminifera.

Ozone depletion: ultraviolet radiation and phytoplankton biology in antarctic waters.

The springtime stratospheric ozone (O3) layer over the Antarctic is thinning by as much as 50 percent, resulting in increased midultraviolet (UVB) radiation reaching the surface of the Southern Ocean. There is concern that phytoplankton communities confined to near-surface waters of the marginal ice zone will be harmed by increased UVB irradiance penetrating the ocean surface, thereby altering the dynamics of Antarctic marine ecosystems. Results from a 6-week cruise (Icecolors) in the marginal ice zone of the Bellingshausen Sea in austral spring of 1990 indicated that as the O3 layer thinned: (i) sea surface- and depth-dependent ratios of UVB irradiance (280 to 320 nanometers) to total irradiance (280 to 700 nanometers) increased and (ii) UVB inhibition of photosynthesis increased. These and other Icecolors findings suggest that O3-dependent shifts of in-water spectral irradiances alter the balance of spectrally dependent phytoplankton processes, including photoinhibition, photoreactivation, photoprotection, and photosynthesis. A minimum 6 to 12 percent reduction in primary production associated with O3 depletion was estimated for the duration of the cruise.

Deep-sea hydrocarbon seep communities: evidence for energy and nutritional carbon sources.

Mussels, clams, and tube worms collected in the vicinity of hydrocarbon seeps on the Louisiana slope contain mostly "dead" carbon, indicating that dietary carbon is largely derived from seeping oil and gas. Enzyme assays, elemental sulfur analysis, and carbon dioxide fixation studies demonstrate that vestimentiferan tube worms and three clam species contain intracellular, autotrophic sulfur bacterial symbionts. Carbon isotopic ratios of 246 individual animal tissues were used to differentiate heterotrophic (8(13)C = -14 to -20 per mil), sulfur-based (8(13)C = -30 to -42 per mil), and methane-based (8(13)C = <-40 per mil) energy sources. Mussels with symbiotic methanotrophic bacteria reflect the carbon isotopic composition of the methane source. Isotopically light nitrogen and sulfur confirm the chemoautotrophic nature of the seep animals. Sulfur-based chemosynthetic animals contain isotopically light sulfur, whereas methane-based symbiotic mussels more closely reflect the heavier oceanic sulfate pool. The nitrogen requirement of some seep animals may be supported by nitrogen-fixing bacteria. Some grazing neogastropods have isotopic values characteristic of chemosynthetic animals, suggesting the transfer of carbon into the background deep-sea fauna.

Enzyme elements involved in the interconversion of L-carbamylaspartate and L-dihydroorotate by dihydroorotase from Clostridium oroticum.

Enzyme elements that are involved in the reversible cyclization of L-carbamylaspartate to L-dihdroorotate catalyzed by dihydroorotase (EC 3.5.2.3) from Clostridium oroticum (ATCC 25750) have been studied. Removal of Zn(II) from the enzyme by chelators followed by incubation of apoenzyme with Co(II) results in replacement of two to three of the four Zn(II) ions per molecule by Co(II). The catalytic properties of the Zn(II)Co(II) dihydroorotase are different from those of native enzyme. The Vmax is increased for both the synthesis and hydrolysis of L-dihydroorotate. The Km for L-dihydroorotate is unchanged, while the Km for L-carbamylaspartate is increased more than twofold. On the other hand, the kinetic properties of Zn(II)-reconstituted dihydroorotase are indistinguishable from those of native enzyme. The pH dependence of Vmax is also altered by the Co(II) substitution. For both Zn(II)- and Zn(II)Co(II)-dihydroorotase, this pH dependence is well described by a single ionization and the pK's for L-dihydroorotate synthesis and hydrolysis are different. Substitution with Co(II) increases the pK for both reaction directions to different extents. These results strongly support a role for the tightly bound metals in the catalytic mechanism. In addition, diethylpyrocarbonate rapidly inactivates the enzyme. The inactivation is prevented by L-dihydroorotate. This result is consistent with a role for at least one histidine in catalysis. The possibility that C. oroticum dihydroorotase may be useful model for the more complex mammalian enzyme is considered.

Evidence for a pH-dependent isomerization of Clostridium oroticum dihydroorotase.

Analytical gel permeation chromatography on both Sephadex and polyacrylamide columns shows that Clostridium oroticum dihydroorotase (L-5,6-dihydroorotate amidohydrolase, EC 3.5.2.3) undergoes a large decrease in molecular size when the pH is decreased from 8 to 6. The Stokes radius decreases from about 40 A to 36 A. Neither the molecular size nor kinetic properties are dependent on protein concentration. Thus, the decreased molecular size reflects a pH dependent isomerization of the enzyme.

Dihydro-orotase from Clostridium oroticum. Purification and reversible removal of essential zinc.

A new purification procedure involving five column-chromatography steps is described for dihydro-orotase (L-5,6-dihydro-orotate amidohydrolase, EC 3.5.2.3) from Clostridium oroticum (A.T.C.C. 25750). The native purified enzyme is a dimer of Mr 102 000 and contains 4.0 +/- 0.3 g-atoms of zinc/mol of dimer. These observations agree with those reported previously [Taylor, Taylor, Balch & Gilchrist (1976) J. Bacteriol. 127, 863-873]. It is conclusively demonstrated that dihydro-orotase is a zinc metalloenzyme. Zinc is reversibly removed by treatment with chelators in phosphate buffer at pH 6.5, as demonstrated by atomic absorption spectrophotometry and decrease of enzyme activity. The specific activity is linearly dependent on zinc content. Addition of ZnSO4 to the chelator-treated enzyme results in regain of the normal complement of zinc and enzyme activity. Kinetic properties of the reconstituted enzyme are indistinguishable from those of the native enzyme. The amino acid composition of the homogeneous enzyme suggests that the zinc atoms occupy different environments.

Silhouette photography of polyacrylamide slab gels.

A silhouette photography technique for making same-size negative films and positive contact prints of Coomassie blue-stained polyacrylamide slab gels is described. This technique does not require expensive photographic equipment and provides the resolution obtained with conventional camera systems.