Coral illumination through an optic glass-fiber: incorporation of 14C photosynthates

The pathways of ¹⁴C incorporation into the three major compartments of the coral body were analysed in colonies of Stylophora pistillata. We used the optic glass-fiber method to carry out two sets of experiments: in the first, 11 different colonies were sampled immediately after incubation; in the second, 3 colonies were returned to the reef at the termination of incubation for a further period of 29 h. Within the tissue compartment, significantly more ¹⁴C labeled products were incorporated into illuminated tips or bases than into unilluminated sections. Tips located above illuminated bases contained amounts of ¹⁴C products similar to unilluminated tips. Within the organic matrix compartment, illumination of tip or base segments again resulted in increased amounts of ¹⁴C fixation, and again unilluminated tips located above the illuminated bases did not accumulate more ¹⁴C photosynthates than other tips on the same branches. The absence of detectable translocation was also confirmed after a post-incubation period of 29 h, and raises questions as to the validity of the widely accepted theory of upward translocation. Within the skeletal carbonate compartment, although the results were associated with a high coefficient of variation, significantly more ¹⁴C accumulated in the tips than in the bases. Illumination of tips or bases did not enhance ¹⁴C uptake. A light-independent carbon assimilation (dark fixation) is significant in S. pistillata within the three tested compartments (the tissue, the organic matrix of the skeleton, and the skeletal carbonate). It is suggested that the dark fixation process in corals in a result of accumulation of respiratory CO₂ and CO₂ from sea water as malate or other titratable acids during the night. During the day these acids are broken down, releasing free CO₂ for C₃ pathway photosynthesis.     

Coral calcification: Sources of error in radioisotope techniques

Isotopic exchange occurs between coral skeleton and ⁴⁵Ca⁺⁺ and H¹⁴CO ₃ ^- in seawater. Exchange of ¹⁴C onto skeletons is more rapid than exchange of ⁴⁵Ca⁺⁺. Exchange of ¹⁴C from skeletons to seawater takes place more slowly than exchange of ⁴⁵Ca⁺⁺ to seawater. When living coral is incubated in the dark with radioisotopes for 1 h, the tissues contain considerably more radioactivity than is associated with the skeleton. The tissue radioactivity reflects permeation of tissues and coelenteron by radioactive compounds from the incubation seawater. Addition of alkalis to cardioactive seawater results in a radioactive precipitate, part of which becomes associated with any coral skeleton present, and part of which forms on the wall of the containing vessel. Strong alkali removes biologically-deposited radioisotope from coral skeletons. Deposition, of ¹⁴C from H¹⁴CO ₃ ^- in skeletons of living coral incubated in the dark is greater than in dead coral. The reverse situation occurs with ⁴⁵Ca⁺⁺.     

Calcification in the staghorn coral Acropora acuminata: Variations in apparent skeletal incorporation of radioisotopes due to different methods of processing

Pieces of branch from the staghorn coral Acropora acuminata were incubated with ⁴⁵CaCl₂ and NaH¹⁴CO₃ under identical conditions in the light or in the dark. Specimens were then processed in different ways. All specimens were placed in N KOH to digest tissues. Some were placed in KOH immediately after incubation; others were placed in KOH after 2 h washing, or after 2 h extraction with methanol-chloroformwater. Specimens were washed in running fresh water or running seawater; some were killed in liquid N₂ before washing. Radioactivity associated with skeleton and tissues was determined. The method of processing profoundly affected the results. In dark incubations, there was up to a four-fold difference in apparent skeletal incorporation of ⁴⁵Ca⁺⁺ between average values obtained for the different treatments. For ¹⁴C incorporation, there was a difference of up to 2.5 times. In light incubations, skeletal incorporation of both radioisotopes showed a two-fold difference between high and low average values obtained for the different treatments.     

Carbon flow into the end-products of photosynthesis in short and long incubations of a natural phytoplankton population

During a cruise to the eastern Canadian Arctic (Northern Baffin Bay) in the summer of 1980, we took advantage of the 24-h photoperiod to conduct a 32-h time course experiment of ¹⁴C accumulation under natural solar radiation. The degree of non-linearity in the time course was judged against a time-dependent curve of radioactivity constructed by cumulatively adding the amount of ¹⁴C taken up in sequential short (2 h) incubations of plankton held in a replicate bottle but left unlabelled until removed for assay. Departure from linearity was due first to decreasing rates of ¹⁴C incorporation into polysaccharides and then into lipids. There was a close correspondence between ¹⁴C incorporation into proteins in the 32-h incubation and in the sequence of short incubations. These observations are consistent with patterns in utilization of photosynthetic end-products established from laboratory studies of unicellular algal cultures. Based on parallel or independent control experiments, it was judged that complicating factors such as diel light changes, nitrogenous nutrient exhaustion, bottle size effects or inhibitory conterminants in NaH¹⁴CO₃ stock solutions would not seriously affect our interpretation that non-linearity resulted from catabolic loss of radiocarbon.     

Turnover of photosynthetically fixed carbon in reef corals

Siderastrea siderea and Montastrea annularis were labeled in situ with NaH¹⁴CO₃. The corals were sampled over a period of 11 days and the radioactivity remaining in the ethanolsoluble and ammonia-soluble fractions measured. Total radioactivity in the corals fell to about 1/3 after one night and then to about 1/3 in the next 10 days. The ethanol-soluble radioactivity is probably converted to the less soluble, ammonia-extractable, material in the dark.Contribution No. 1514 from the University of Miami, Rosenstiel School of Marine and Atmospheric Science, 10 Rickenbacker Causeway, Miami, Florida 33149, USA.     

Effects of dissolved ammonium addition and host feeding with Artemia salina on photoacclimation of the hermatypic coral Stylophora pistillata

 Effects of nutrient treatments on photoacclimation of the hermatypic coral Stylophora pistillata (Esper) were studied. Studies on photoacclimation of colonies from different light regimes in the field were evaluated and used to design laboratory experiments. Coral colonies were collected in the Gulf of Eilat (Israel) from January to March 1993. Exterior branches of colonies from different depths (1 to 40 m) displayed different trends in production characteristics at reduced and very low levels of illumination. From 24 ± 3% to 12 ± 2% of incident surface photosynthetic active radiation (PAR_o), zooxanthella population density and chlorophyll a+c per 10⁶ zooxanthellae increased, a trend seen in the range of light levels optimal for coral growth (90 to 30% PAR_o). The P _max of CO₂ per 10⁶ zooxanthellae decreased, while P _max of CO₂ per 10³ polyps increased, indicating an increase in zooxanthella population density at low light levels. Proliferous zooxanthella frequency (PZF, a measure of zooxanthella division) declined significantly at light levels <18 ± 3% PAR_o. At the lowest levels of illumination (<5% PAR_o), zooxanthella population density decreased, as did the PZF; chl a+c per 10⁶ zooxanthellae was unchanged. In 28-d experiments, exterior coral branches from the upper surfaces of colonies from 3 m depth (65 ± 4% PAR_o) were incubated in aquaria under bright (80 to 90% PAR_o), reduced (20 to 30% PAR_o), and extremely low (2 to 4% PAR_o) light intensities. At each light intensity, the corals were maintained in three feeding treatments: sea water (SW); ammonium enriched SW (SW + N); SW with Artemia salina nauplii (SW + A). An increase in P _max of CO₂ per 10³ polyps was found in corals acclimated to reduced light (20 to 30% PAR_o) in nutrient-enriched SW, while in SW, where the increase in zooxanthella population density was smaller, it did not occur. Nutrient enrichments (SW + N at 2 to 4% PAR_o and SW + A at 20 to 30% PAR_o) increased zooxanthella population density, but had no effect on chl a+c per 10⁶ zooxanthellae. Acclimation for 14 d to reduced (10 to 20% PAR_o) and extremely low (1 to 3% PAR_o) light intensities shifted ¹⁴C photoassimilation into glycerol and other compounds (probably glycerides), rather than sugars. Both ammonium addition and feeding with Artemia salina nauplii resulted in an increase in photosynthetic assimilation of ¹⁴C into amino acids. We conclude that acclimation to reduced light consists of two processes: an increase in photosynthetic pigments and in zooxanthella population density. Both processes require nitrogen, the increase in zooxanthella population density needing more; this adaptation is therefore limited in nitrogen-poor sea water. Received: 19 June 1998 / Accepted: 13 June 2000     

Photorespiration and productivity rates of a coral reef algal turf assemblage

In studies conducted from 1982 to 1983, productivity (¹⁴C uptake) of a coral reef algal-turf assemblage was unaffected by oxygen concentration but decreased when pH rose, probably in response to declining CO₂ and HCO ₃ ^- supplies. Release of prefixed ¹⁴C was substantially lower in the light than in the dark and was unaffected by oxygen concentration. Release of organic prefixed ¹⁴C was greater in the light than in darkness. Total CO₂ compensation-points were low, showing no consistent response to oxygen or the photorespiratory inhibitor alpha-hydroxy-2-pyridine-methanesulfonic acid (HPMS). Oxygen has little if any influence upon turf productivity, which was high in comparison to other benthic algae. Decreases in net carbon-fixation rates of this turf more likely result from decreased photosynthesis than increased photorespiration, which is either not significant in turf metabolism under natural conditions or is compensated by efficient refixation of respired carbon.This paper describes research by J. M. Hackney in partial fulfillment of the requirements for the Ph.D. degree at Georgetown University     

Metabolic disposition of lactate in the horseshoe crab Limulus polyphemus and the stone crab Menippe mercenaria

The metabolism of ¹⁴C-labelled lactate was investigated in the horseshoe crab Limulus polyphemus and the stone crab Menippe mercenaria. When a bolus of (¹⁴C-U)-D-lactate was injected into L. polyphemus, there was substantial release pf ¹⁴CO₂ into the medium. In the case of M. mercenaria, ¹⁴CO₂ release was also observed after injection of (¹⁴C-U)-L-lactate into experimental individuals. Analysis of the distribution of radioactivity in whole body extracts of both species revealed easily detectable amounts of radioactivity in the glycogen fraction, although the bulk of the radioactivity was in the cation, anion/neutral and CO₂ fractions. To investigate the metabolism of lactate further, ¹⁴C-labelled lactate was injected into large individuals of L. polyphemus and M. mercenaria, and the distribution of radioactivity was determined in the hemolymph, muscle and hepatopancreas. Utilization of (¹⁴C-U)-D-lactate by L. polyphemus resulted in the accumulation of significant amounts of labelled glucose in all three body compartments as well as the production of labelled glycogen in the telson levator muscle and hepatopancreas. Utilization of (¹⁴C-U)-L-lactate resulted in a similar pattern of glucose and glycogen labelling in the hemolymph, cheliped muscle and hepatopancreas of M. mercenaria. These studies demonstrate that both L. polyphemus and M. mercenaria have the capacity for glyco- and gluconeogenesis using lactate as the substrate.     

A reevaluation of the role of glycerol in carbon translocation in zooxanthellae-coelenterate symbiosis

Glycerol has been traditionally viewed as the main form of carbon translocated from zooxanthellae to the coelenterate host. Most of this glycerol was postulated to be used by the coelenterate host for lipid synthesis. Recent work suggests that large amounts of photosynthetically fixed carbon is synthesized into lipid in the algae, and then translocated as lipid droplets to the host. These two hypotheses of carbon translocation are not mutually exclusive, but to reconcile them the role of glycerol must be reevaluated. In this study the short term metabolic fate of uniformly labelled ¹⁴C-glycerol, ¹⁴C-bicarbonate, and ¹⁴C-acetate was examined in zooxanthellae and coelenterate host tissue isolated from Condylactis gigantea tentacles. When host and algal triglycerides, synthesized during 90-min light and dark incubations in ¹⁴C-bicarbonate and ¹⁴C-acetate, were deacylated, more than 80% of the activity was found in the fatty acid moiety. In contrast, triglycerides isolated from zooxanthellae and coelenterate host tissue incubated in ¹⁴C-glycerol in the dark for 90 min were found to have more than 95% of their radioactivity in the glycerol moiety. During the 90-min ¹⁴C-glycerol incubations in the light, the percentage of radioactivity in the fatty acid moiety of zooxanthellae triglycerides increased to 37%. The percentage of radioactivity in the host tissue triglycerides fatty acid moiety stayed below 5% during the 90-min ¹⁴C-glycerol incubations in the light. These results show that neither the zooxanthellae nor the host can rapidly convert glycerol to fatty acid. Radioactivity from ¹⁴C-glycerol, which does eventually appear in host lipid, may have been respired to ¹⁴CO₂, then photosynthetically fixed by the zooxanthellae and synthesized into lipid fatty acid.     

Habitat preferences of coral-associated fishes are altered by short-term exposure to elevated CO2

Rising atmospheric carbon dioxide (CO₂) concentrations are causing additional CO₂ to be absorbed by the oceans. Recent studies show that exposure to elevated CO₂ causes olfactory impairment in reef fishes; however, the ecological consequences of this impairment are largely unknown. This study examined the effects of short-term exposure to elevated CO₂ on habitat preferences of coral-dwelling gobies. Adult gobies collected from the reef at Lizard Island (Great Barrier Reef, Australia) were exposed for 4 days to ambient CO₂ (440 μatm) or elevated CO₂ (880 μatm). Habitat preferences were then tested in laboratory and field experiments at ambient conditions. In olfactory preference tests, Paragobiodon xanthosomus displayed a strong preference for odour cues of their sole host coral Seriatopora hystrix; however, this preference was absent in gobies exposed to elevated CO₂. Habitat choice experiments conducted in the field showed that Gobiodon histrio placed on dead coral colonies located preferred live habitat within 24 h; however, gobies exposed to elevated CO₂ associated with both preferred and non-preferred habitats in approximately equal frequency. Preferred habitats are known to confer fitness advantages to coral-dwelling gobies. Consequently, these results suggest that future elevated CO₂ levels might affect the ability of habitat specialist fishes to select favourable habitats.     

Lipolytic activity of marine bacteria. Influence of NaCl and MgCl2

A method for the determination of volatile fatty acids (VFA) in coastal marine sediments is presented. Acidified porewater was vacuum distilled to extract the VFA and the distillate was analysed by gas chromatography (Porapak QS column and flame ionization detection). The limit of detection was 2 M in the samples, but was increased tenfold by lyophilization. In the upper 10 cm of the sediments 2–70 nmol acetate cm^-3 sediment was found. Uniformly labelled ¹⁴C-acetate (0.02 nmol, 10^-3 ci) was injected at 1- to 2-cm intervals through silicone-stoppered holes in the tubing of undisturbed sediment cores. Turnover rate constants were determined from semilogrithmic plots of the ¹⁴C-acetate radioactivity versus the incubation time. The ¹⁴C-acetate was shown to be distributed in at least three sediment pools: a porewater pool, an adsorbed pool which was displaced by excess acetate, and an adsorbed pool which was not displaced by excess acetate. The rate constants ranged from 1.5–13 h^-1 in the investigated sediments. The turnover rates of acetate were calculated from the turnover rate constants and the acetate concentrations in the porewater. The rate of acetate turnover calculated from the NH ₄ ^* turnover and the N:C ratio of the sediment organic matter was only 16% of the measured rate of acetate turnover. The apparent overstimation of the acetate turnover was most likely due to an overestimation of the degradable acetate pool. A gel filtration of ¹⁴C-acetate-containing porewater showed that the fractions which contained the tracer had only 25% of the total acetate. This implied that a large fraction of the acetate in the porewater was unavailable to the microbes. This was also indicated by the fact that the measured acetate pool in porewater incubated with ¹⁴C-acetate did not decrease, when the added ¹⁴C-acetate was oxidized.     

Utilization of a fumigated sediment by two benthic deposit-feeders:Abra alba (Mollusca: Bivalvia) andEupolymnia nebulosa (Annelida: Polychaeta)

The present study tested the utilization of dead microbial biomass by two benthic deposit-feeders:Abra alba (Wood) (Mollusca: Bivalvia) andEupolymnia nebulosa (Montagu) (Annelida: Polychaeta). Clams were collected in the Canet lagoon during spring 1989. Worms were collected in the Port-Vendres harbour during spring 1989. The¹⁴C-labelled (glutamic acid, 24 h) sediment used during the study was sterilized with 1% chloroform, washed with sterile seawater, and dried (60°C; 48 h). This sterilisation procedure, called fumigation is the least harmful to the sediment (Novitsky 1986). Both clams and worms were incubated in the presence of the fumigated sediment for 5, 10, 20, and 50 h. At the end of each experiment we recorded the radioactivity in four compartments: (1) sediment, (2) dissolved organic matter (DOM), (3) CO₂, and (4) animals. The radioactivity of the sediment was subdivided into five fractions: (i) soluble in 2N HCl, (ii) soluble in hot 5% trichloroacetic acid (TCA), (iii) soluble in 1N NaOH, (iv) soluble in hot 6N HCl, (v) residual (after combustion in a Leco carbon analyser). In the first set of experiments, after 20 h of incubation, 5.4 and 4.7% of the total radioactivity was taken up by clams and worms, respectively. However, a model revealed that this uptake could have been correlated with the release of radiolabelled DOM (33% of total radioactivity during the first 5 h). In order to test this assumption, we used the same protocol with three additional washes of the fumigated sediment. This resulted in a significantly lower uptake by the clams (1.9% of the total radioactivity byt = 50 h), whereas the worms exhibited an uptake similar to that in the initial experiment (5.1% of total radioactivity byt = 50 h). These results underline the importance of considering interactions with DOM when applying radiotracer techniques to the study of benthic food chains. The average ingestion rates of fumigated sediment byA. alba andE. nebulosa were 5.2 10^–2 mg sediment dry wt mg^–1 clam h^–1 and 3.5 10^–2 mg sediment dry wt mg^–1 worm h^–1, respectively, which is comparable to previous data reported for other deposit-feeding bivalves and polychaetes feeding on natural sediment or detritus. The low radioactivity recorded for CO₂ together with the similarity of the changes in the partitioning of the radioactivity within the sediment between control experiments and experiments carried out in the presence of clams or worms suggest low assimilation efficiencies. Therefore, the present study supports the fact that dead microbial biomass does not constitute an important food source for benthic deposit-feeders.     

Extension rate: A primary control on the isotopic composition of West Indian (Jamaican) scleractinian reef coral skeletons

Large variations in skeletal microarchitecture, and in the carbon and oxygen isotopic composition of the skeleton, exist within single calices and over the surfaces of single colonies of various species of West Indian (Jamaican) scleractinian reef corals. Rapidly extending parts of individual colonies are depleted in both C¹³ and O¹⁸ regardless of the abundance of zooxanthellae in the overlying tissues. We suggest that this relationship is due to active translocation of organic compounds to sites of rapid calcification. Considerable variation in isotopic composition is found in skeletons of different specimens of the same species even when the skeletons are sampled in a consistent manner, come from the same locality and depth, and have a comparable growth history. The isotopic composition of the scleractinian skeleton is vastly more complex than has heretofore been realized.     

Activation energy for skeletal aragonite deposited by the hermatypic coral Platygyra spp.

Average radial growth rates of the hemispherical aragonite colonies deposited by the Indo-Pacific scleractinian reef coral Platygyra spp. were determined by measuring the thickness of density variations in the skeleton that are revealed by X-radiography. Ninety-one specimens from 21 localities were examined, but only 54 of these exhibited well-defined growth-banding. The apparent temperature dependence of growth rate is linear over the range 23.9° to 29.3°C, averaging 5.4±0.94 mm/year at 24°C, 8.0±0.42 mm/year at 27°C, and 9.7 ±0.58 mm/year at 29°C (90% confidence limits). Expression of the influence of temperature on growth rate in terms of the Arrhenius equation yields an activation energy of 20,680 cal/mole, which is comparable to values for typical biological reactions, but is only half that reported for skeletogenesis in another reef coral, Pocillopora damicornis, on the basis of controlled incubation studies involving ⁴⁵Ca uptake.     

Low molecular-weight factor from Plesiastrea versipora (Scleractinia) that modifies release and glycerol metabolism of isolated symbiotic algae

When symbiotic dinoflagellate algae (Symbiodinium sp., isolated from the coral Plesiastrea versipora) were incubated with NaH¹⁴CO₃ in the light in seawater, they released 22.69±9.16 nmol carbon/10⁶ algae. Release of photosynthetically fixed carbon was stimulated more than six-fold for algae incubated in host-tissue homogenate (148.54±97.03 nmol C/10⁶ algae) and more than four-fold (102.00±49.16 nmol C/10⁶ algae) for algae incubated in a low molecular weight fraction (≤1 000 M _r ) prepared from host homogenate. Soluble released ¹⁴C-labelled products, as determined by chromatography and autoradiography, were the same when algae were incubated in either host homogenate or the low molecular weight fraction. After 4 h incubation in the light (300 mol photons m⁻² s⁻¹),␣intracellular␣glycerol increased in algae incubated with the low molecular weight fraction (an increase of 0.39 to␣0.67 nmol glycerol/10⁶ algae) compared with little or no increase in algae incubated in seawater (0 to 0.12 nmol glycerol/10⁶ algae). Partial inhibition of triglyceride synthesis (up to 51%) was also observed when algae were incubated in the low molecular weight fraction. All these effects are the same as those observed when algae were incubated in host homogenate. These data indicate that the “host release-factor” activity of P.␣versipora is a compound of low molecular weight. Received: 13 February 1997 / Accepted: 24 October 1997     

The pattern of carbon fixation in the marine unicellular alga Phaeodactylum tricornutum

The short- and long-term fixation of ¹⁴CO₂ by Phaeodactylum tricornutum was studied using methods of fractionation that allowed examination of all the products labelled with ¹⁴C. There was no doubt that the major pathway of CO₂ fixation was into 3-phosphoglycerate, but there was also significant incorporation by -carboxylation by means of phosphoenol-pyruvate carboxylase and transamination into aspartate. At short time intervals (10 sec), 90% of the radioactive products found were accounted for by 3-phosphoglycerate and aspartate. The lipids associated with the photosynthetic apparatus contained a high proportion of the ¹⁴C fixed, which at 60 sec was located mainly in the carbohydrate portion of the lipids. At 30 and 300 min, the chlorophylls, carotenoids and the long-chain fatty acids were heavily labelled with ¹⁴C. The monogalacto-diglycerides, the digalacto-diglycerides and the sulpholipids each had a characteristic long-chain fatty acid composition. The cell proteins and a reserve polysaccharide were also labelled with ¹⁴C at short time intervals and increased their radioactivity in a linear fashion up to the longest period studied, 300 min. The activity of the enzymes ribulose diphosphate carboxylase and phosphoenolpyruvate carboxylase was sufficient to account for the pattern of fixation found.     

Amino acid synthesis in the symbiotic sea anemone Aiptasia pulchella

Symbiotic Aiptasia pulchella and freshly isolated zooxanthellae were incubated in NaH¹⁴CO₃ and NH₄Cl for 1 to 240 min, and samples were analysed by reverse-phase high-performance liquid chromatography (HPLC) and an online radiochemical detector. NH₄ ⁺ was first assimilated into ¹⁴C-glutamate and ¹⁴C-glutamine in the zooxanthellae residing in A. pulchella. The specific activities (dpm nmol⁻¹) of ¹⁴C-glutamate and ¹⁴C-glutamine in vivo, were far greater in the zooxanthellae than in the host tissue, indicating that NH₄ ⁺ was principally incorporated into the glutamate and glutamine pools of the zooxanthellae. ¹⁴C-α-ketoglutarate was taken up from the medium by intact A. pulchella and assimilated into a small amount of ¹⁴C-glutamate in the host tissue, but no ¹⁴C-glutamine was detected in the host fraction. The ¹⁴C-glutamate that was synthesized was most likely produced from transamination reactions as opposed to the direct assimilation of NH₄ ⁺. The free amino acid composition of the host tissue and zooxanthellae of A. pulchella was also measured. The results presented here demonstrate that NH₄ ⁺ was initially assimilated by the zooxanthellae of A. pulchella. Received: 3 February 1997 / Accepted: 24 October 1997     

14C of grasses as an indicator of fossil fuel CO2 pollution

Measuring the amount of fossil fuel carbon stored in the vegetation is now crucial to understand the mechanisms ruling climate changes. In this respect, highly polluted areas such as major towns represent “natural” laboratories because fossil fuel CO₂ (¹⁴C-free) is isotopically distinct from mean atmospheric CO₂ (¹⁴C-labeled). Here, a¹⁴C study of urban grasses near a major highway in Paris, France, shows that plants store up to 13% of fossil fuel carbon. The ¹⁴C composition of urban grasses is thus a novel parameter to assess the fossil fuel CO₂ pollution.     

Pharmacokinetics of [14C]-atrazine in rhesus monkeys,single-dose intravenous and oral administration

This is the first study regarding the pharmacokinetics of [¹⁴C]-atrazine conducted with rhesus monkeys. The animals received one dose (0.25 mg) intravenously (IV) or three doses (1, 10, or 100 mg) orally. Plasma, urine, and feces were collected at defined times up to 7 days post-dosing. Sample radioactivity was measured to determine the mass equivalent. IV administered [¹⁴C]-atrazine disappeared rapidly from blood, with an elimination half-life of about 5.5 ± 1.1 h. The pharmacokinetic profiles of [¹⁴C]-atrazine following oral administration at the three dose levels show that kinetic parameters such as AUC and C _max are linearly correlated with the dose. Seven days after dosing, urinary and fecal excretion of [¹⁴C]-atrazine reached 99% of total administered dose in the IV group and 91–95% in the three oral dose groups. In the IV-administered monkeys, approximately 85% of the dose was excreted in urine and 12% in feces. In three oral dose groups, urinary and fecal radioactivity recoveries approximated 57% and 21%, 58% and 25%, and 53% and 35%, respectively. More than 50% of the total urinary excreted radioactivity was found within the first 24 h after dosing. In conclusion, the principal elimination of [¹⁴C]-atrazine, IV and orally administered, is via urine. The oral bioavailability was 60% or higher. There was a significant linear correlation between administered oral dose and plasma concentration. Overall oral dose accountability ranged from 91% to 95%. Data generated may be useful in the risk assessment of human exposure to environmental atrazine contamination.     

Reproductive success in the Caribbean octocoral Briareum asbestinum

For most sessile marine invertebrates the number of offspring produced by an individual is often determined indirectly from counts of eggs present, with the assumption that all or most become viable offspring. Few field data on the actual number of offspring produced per individual (reproductive success) have been reported. We examined reproductive success in the octocoral, Briareum asbestinum (Pallas), by measuring embryo densities on 40 female colonies on two reefs (Pinnacles and House reefs) in the San Blas Islands, Panama from 1986 to 1988. The percentage of female colonies with mature eggs which subsequently released embryos was low, ranging from 46.6% in 1986 to 5.0% in 1988. Reproductive success was significantly different between reefs. Pinnacles reef had significantly more successful colonies (those releasing embryos) than House reef in all three years and significantly higher embryo densities in 1986 and 1987. There was a significant positive correlation between female reproductive success and the density and proximity of nearby males in both 1986 and 1987. In addition, fertile female branches placed 25 cm away from male branches produced significantly more embryos than female branches placed 50 cm away. In 1988 two groups of female branches were placed at distances of <50 cm and 5 m from four large male colonies at Pinnacles reef. Of the 20 female branches placed 5 m from the males none released embryos while 35% (7 of 20 branches) of the branches <50cm from males released embryos. These data indicate that simple counts of mature eggs present within female colonics prior to the reproductive season provide a poor estimate of reproductive success in B. ashestinum and that female reproductive success is positively influenced by the close proximity of males.