Analyse von Wachstumskurven von Heterostegina depressa (Foraminifera: Nummulitidae)

Chamber formation in individuals of the large foraminifer Heterostegina depressa was studied with the intention of explaining the different shapes of growth curves established for groups of individuals. The material was derived from clone cultures and from the natural habitat. Chamber formation was observed by daily control of many individuals. The growth increments of a group of individuals depend mainly upon the frequency of chamber formation of the individuals, they also depend upon the percentage of growing individuals present and the sizes of chambers. Within a prolifically growing group, each individual builds a new chamber every second or third day, and 81 to 86% exhibit chamber-building activities. Further features of quickly growing individuals are: formation of chambers in a regular sequence, and short periods of rest between long periods of growth. During low illumination intensity and in darkness, growth of H. depressa may cease for several months (up to 81/2 months). Cessation of growth is connected with a marked reduction in all other physiological processes. After month-long inhibition of growth, different individuals responded with different growth behaviour under the same environmental conditions. For example, smaller individuals needed longer periods of physiological regeneration before building new chambers. Prior darkexposure resulted in intermittent growth in many individuals. Periods of rest were followed by periods of unusually intensive growth. Lower temperature resulted in a reduced frequency of chamber formation. The size of chambers, however, was not influenced; accordingly the shape of the test did not vary. Immediately after multiple fission, rapid growth begins. Growth curves of H. depressa, therefore, do not show initial periods of slow growth which is characteristic for general exponential growth. H. depressa exhibited sigmoidal growth curves only after periods of growth inhibition; it displayed typical regenerative growth. During these periods, up to 4 chambers in 4 days, or 9 chambers in 12 days, were built by 11-month-old individuals.     

Die Ektoplasmahülle von Heterostegina depressa (Foraminifera:Nummulitidae)

The structure of the rigid ectoplasm sheath was studied in living individuals of the large foraminifer Heterostegina depressa d'Orbigny 1826 (Nummulitidae). H. depressa is able to form pseudopods, which emerge from the marginal cord within a few minutes. Normally, however, the living test is entirely covered by a rigid hyalin elastic sheath, which is fixed to the substrate by terminally branched processes. In older individuals, the sheath is often incomplete and restricted to the marginal cord only. Probably, the sheath is secreted by the ectoplasm which fills the canal system of the chamber walls and the marginal cord, or it consists of transformed ectoplasm; we call it “Ektoplasmahülle”, and the processes radiating to all sides, “Ruhepseudopodien”. H. depressa is able to move while inside the elastic sheath by means of pseudopods which penetrate the sheath and attach themselves to the substrate out-side. In the same manner, H. depressa leaves a complete sheath by disrupting it through the tractive powers of the pseudopods. The procedure of breaking the sheath is described. Locomotion when leaving the sheath is performed in a zigzag manner (alternating action of several pseudopods). The sheath counteracts transportation by water movement and protects chamber formation (which takes place inside the sheath). Due to its symbiotic unicellular algae, H. depressa does not need to collect food particles; hence locomotion seems unneccssary. The formation of a rigid ectoplasm sheath may be connected with H. depressa's sessile mode of life.     

Larger foraminifera: Reproduction and early stages of development in Heterostegina depressa

The process of reproduction (multiple fission) of the megalospheric gamont of Heterostegina depressa d'Orbigny, 1826 (Nummulitidae) is described. During this process, the protoplasm separates outside the parent test into the juveniles. The initial chambers receive some of the symbiotic algae from the parent protoplasm. The second chamber develops from the initial chamber by division, not by growth. The newly formed 2-chamber-stage receives a second set of symbiotic algae from the parent residual protoplasm. Thereafter, calcification takes place, and the first ectoplasm sheath is formed. The problem of alternation of generations is discussed. From the very small proportion of microspheric individuals found in Heterostegina species (fossil and recent) it is concluded that gamogony has been greatly reduced.     

Light absorption,photosynthesis and growth of Nannochloris atomus in nutrient-saturated cultures

Nannochloris atomus was maintained in exponential growth at photon flux densities (PFD) from 400 to 700 nm, ranging from 10 to 200 mol m^-2 s^-1. Growth was lightsaturated at PFDs in excess of 100 mol m^-2 s^-1, with a mean light-saturated growth rate at 23 °C of 1.5×10^-5s^-1 (1.2 d^-1). The light-limited growth rates extrapolated to a compensation PFD for growth that was not significantly different from zero, although no changes in cell numbers were observed in a single culture incubated at a PFD of 1.0 mol m^-2s^-1. Dark-respiration rates were independent of PFD, averaging 1.7×10^-6 mol O₂ mol^-1 C s^-1 (0.14 mol O₂ mol^-1 C d^-1). The maximum photon (quantum) efficiency of photosynthesis was also independent of PFD, with a mean value of 0.12 mol O₂ mol^-1 photon. The chlorophyll a-specific light absorption cross-section ranged from 3 to 6×10^-3 m² mg^-1 chl a and was lowest at low PFDs due to intracellular self-shading of pigments associated with high cell-chlorophyll a contents. The C:chl a ratio increased from 10 to 40 mg C mg^-1 chl a between PFDs of 14 and 200 mol m^-2 s^-1. These new observations for N. atomus are compared with our previous observations for the diatom Phaeodactylum tricornutum in terms of an energy budget for microalgal growth.     

Distribution of the marine littoral Foraminifera in Argentina,Uruguay and Southern Brazil

Benthic foraminifers collected in the marine littoral zone (sensu lato) of Argentina, Uruguay and Southern Brazil have been studied and compared with the Foraminifera collections from the same area studied previously. Two figures have been prepared, which show the geographical range and relative abundance of the most important species (cosmopolitan and non-cosmopolitan). The following biogeographical conclusions were drawn on the basis of an analysis of these figures. The whole area, from a latitude of about 32° S up to the southern coast of Tierra del Fuego, should be considered as one biogeographical unit (a kingdom of Buccella peruviana, sensu lato). This unit has 2 internal boundaries, which are located approximately at latitudes 41° and 52° S. They divide the whole area into 3 sub-areas which can be called (from North to South): North Patagonian (32° to 41° S), South Patagonian (41° to 52° S) and Malvinian (52° S—southern coast of Tierra del Fuego). With the exception of Buccella peruviana, sensu lato, which is typical of all 3 sub-areas, these sub-areas are characterized by the following faunal features. The North Patagonian sub-area contains abundant numbers of Elphidium discoidale. The South Patagonian sub-area is characterized by abundant numbers of Elphidium macellum. The Malvinian sub-area contains abundant numbers of Elphidium macellum, and also several very typical representatives of the Malvin current water, for instance, Cassidulina crassa, sensu stricto, Angulogerina angulosa, Uvigerina bifurcata, Cassidulinoides parkerianus, Ehrenbergina pupa and others. It is a matter of opinion whether the sub-areas cited be considered biogeographical sub-provinces, or even smaller units. They cannot be interpreted as biogeographical provinces.Contribution No. 62 of the Puerto Deseado Marine Biological Station.     

Marine fungi (Ascomycetes) within and on tests of Foraminifera

Fruiting bodies of higher marine fungi occur within and on tests of foraminiferans on tropical beaches of the Pacific (Australia, Hawaii) and Atlantic Ocean (Belize, Mexico). Ascocarps (fruiting bodies ) of five intertidal species or varieties of the genera Arenariomyces, Corollospora and Lindra colonize foraminiferans in the natural habitat and may contribute to the eventual breakup of the tests. Fungal fruiting structures, which are normally subglobose when developing in other substrates, adjust to the shape of the foraminiferan chambers when growing within the tests. Pure cultures of L. thalassiae var. crassa yielded the same type of irregular fruiting bodies when grown at 30° C on foraminiferan tests as the sole source of nutrients.Smithsonian Contribution No. 174 (Investigations of Marine Shallow-Water Ecosystems Program, Reef and Mangrove Study-Belize)     

Benthic polychaetes in the Ratnagiri bay, India: influence of anthropogenic factors

Study of changes in macrobenthic community structure is an intrinsic part of many environmental monitoring programmes. Hence, it is pivotal to distinguish the effects of natural and anthropogenic factors on these sensitive organisms for accurate assessment and management of coastal environment. Polychaete species diversity of five stations in the Ratnagiri bay was investigated during premonsoon and postmonsoon months in 2007. Though no spatial trends in polychaete diversity vis-à-vis the pollution was visible, the polychaete univariate indices were uniformily better in premonsoon indicating clear seasonal trends. Shannon diversity values ranged from 1.4-2.4 during premonsoon and 0.6-1.6 during postmonsoon. Station 5, which was most impacted by anthropogenic wastes as demonstrated by the anoxic conditions coupled with higher nutrient load, had comparatively higher H' values (1.9 and 1.6) and better evenness values (0.9 and 0.7) during both seasons indicating that the polychaetes were not influenced by anthropogenic contamination. The study indicates that the polychaete distribution and diversity in the bay were governed primarily by variations in sediment texture rather than the anthropogenic disturbances.     

Benthic response to sedimentation of a spring phytoplankton bloom: Process and budget

The response of benthos to sedimentation of the spring phytoplankton bloom in the Kiel Bight (Western Baltic Sea) is described in terms of biomass (ATP) and activity (heat production and ETS-activity). Input of the bloom (11.5 g C m^-2) over a period from March 25 to April 19, 1980 to the sediment surface was in the form of cells and fresh phytodetritus as indicated by low C/N ratios (7) and high energy charge values (0.78). Benthic microbial activity was immediately stimulated by this input as heat production doubled and the activity of ETS tripled over winter values within 12 d in the absence of a significant increase in ambient temperature. A comparison of the two activity parameters suggests that anaerobic metabolism is more important during the winter (February and March) than after input of the bloom. Meiofauna was not able to take part in the first activity outburst. Benthic ATP-biomass (excluding macrofauna) doubled in late April due to microbial production, and doubled again in early May when meiofauna started reproductive activity. For macrofauna a general statement was not possible, although the sediment surface feeder Macoma baltica commenced a build up of glycogen and lipid resources immediately following bloom input whereas Nephtys ciliata, feeding on sediment and small macrofauna, showed a less pronounced and delayed effect from this input. An energy budget based on heat production measurements was calculated. A daily heat loss of the benthic community of 21.7 KJ m^-2 d^-1 (35.5 KJ m^-2 d^-1) was found, when a depth of 3 cm sediment (5 cm) was assumed. Heat production of macrofauna contributed less than 5% of this activity. The input of the bloom was burned within 21 (13) d. Preliminary estimations for an annual budget suggest that the vertical transport of particulate organic matter via sedimentation can only explain 25% (15%) of the benthic activity in the shallow water ecosystem of the Kiel Bight. This indicates the presence of other sources of organic carbon such as benthic primary production or other transport processes providing carbon to the sediments.Publication No. 384 of the Joint Research Program of Kiel University (Sonderforschungsbereich 95)     

Benthic diversity gradients and shifting baselines: implications for assessing environmental status

The increasing pressure on marine biodiversity emphasizes the importance of finding benchmarks against which to assess change. This is, however, a notoriously difficult task in estuarine ecosystems, where environmental gradients are steep, and where benthic biodiversity is highly variable in space and time. Although recent emphasis on diverse, healthy benthic communities in legislative frameworks has increased the number of indices developed for assessing benthic status, there is a lack of quantitative baselines in benthic diversity that would enable comparisons across broad spatial scales, encompassing different environmental settings and bioregions. By taking advantage of long-term monitoring data, spanning hundreds of stations over the past 40 years, we provide a comprehensive analysis of benthic a, beta, and gamma diversity, encompassing the entire' salinity gradient of the open sea areas of the large, brackish-water Baltic Sea. Using a relatively simple measure, average regional diversity, we define area-specific reference conditions and acceptable deviation against which to gauge current conditions in benthic macrofaunal diversity. Results show a severely impaired condition throughout large areas of the Baltic for the assessment period 2001-2006. All ecosystems are plagued by baselines that shift in time and space, and their definition is not trivial, but average regional diversity may offer a transparent way to deal with such changes in low-diversity systems. Identifying baselines will be of increasing importance given the potential of climatic drivers to interact with local anthropogenic stressors to affect patterns of biodiversity. Our analysis provides an evaluation of the current condition in a system that has been heavily influenced by anthropogenic impact and changing oceanographic conditions, and it provides a basis for future impact assessment and ecosystem-based management.     

Benthic Fluxes and Pore Water Profiles in the Tigullio Gulf

Diffusive fluxes of elements (NO^-₂, NO^-₃, NH⁺₄, SiO₂, PO^3-₄, Cl^-, SO^2-₄, Fe, Mn) have been measured by applying the Fick's first law in two stations of the Tigullio Gulf: the first one characterized by sandy sediments rich in vegetal detritus and the second one, located to within the tourist harbour, characterized by a silty-clay sediments.

Benthic fluxes were measured only in the second station by means of benthic chamber experiments. Although the significant presence of dissolved oxygen in the surface sediments, and the evidence of processes usually occurring in oxidised sediments such as nitrification, both stations also presented characteristics of anoxic sediments such as high oxygen consumption rate and high pore water concentrations of ion, manganese and N-ammonia and reactive orthophosphate.

In both stations, sediments seemed to represent a potential source for most of the chemical species studied, although fluxes were not confirmed for ion, manganese and reactive orthophosphate in benthic chamber experiments.

Diffusive fluxes presented a general agreement for both stations, with higher fluxes of N-nitrate and N-nitrite at the first station were oxidative processes of N-ammonia in the upper layer of the sediments seemed to be more active. the comparison between diffusive and benthic fluxes showed a possible contribution of bioturbation.     

Trace Metal Distribution and Enrichment in Benthic, Estuarine Sediments: Southport Broadwater, Australia

The distribution and enrichment of selected trace metals (Cd, Cr, Cu, Ni, Pb, Sn, Zn) in benthic sediments of the Southport Broadwater, a semi-enclosed coastal body of water adjacent to the Gold Coast city, south-eastern Queensland, Australia, was studied with the objective of assessing the extent and degree of sediment contamination. Sediment samples from the 0–10 cm and 10–20 cm depth intervals of 32 sites within the Southport Broadwater and surrounding residential canals were analysed for particle size distribution, pH, organic C and ‘near-total’ major (Al, Ca, Fe, Mn) and trace (Cd, Cr, Cu, Ni, Pb, Sn, Zn) metal contents. Sediment contamination for each trace metal was assessed by (1) comparison with Australian sediment quality guidelines, (2) calculation of the index of geoaccumulation based on regional background values, and (3) geochemical normalisation against Al (i.e. the abundance of alumino-silicate clay minerals). Based on this approach, the results indicate that submerged sediments in the study area are not presently enriched with Cd, Cr or Ni, with the spatial distribution of these metals being very well explained by the abundance of alumino-silicate clay minerals. However, several sites were strongly enriched with Cu, Pb, Sn and Zn, arising from sources related to either urban runoff or vessel maintenance activities. The study indicates that several varying approaches are needed for a satisfactory assessment of contaminant enrichment in estuarine sediments.     

Community Experiments Using Benthic Chambers: Microbial Significance in Highly Organic Enriched Sediments

The structure of the benthic microbial loop was studied in order to understand heterotrophic pathways in the suboxic sediments of the Rapallo Harbour in autumn, 1996. Sediments were characterized by the large accumulation of organic detritus (17.2 - 21.4 μg chloroplastic pigment equivalents (CPE)g^-1; carbohydrates and proteins: 7.8-16.7 and 6.7-7.5 mg g^-1). Due to the high organic load, benthic bacteria and protozoa displayed extremely high densities (1.4 × 10⁹ cells g^-1 and 26.9 × 10⁵ cells g^-1). Meiofauna, protozoa and bacteria showed an approximate biomass ratio of 1:2:20. the presence of large amounts of organic matter appeared to determine a shift of the benthic size structure toward the increasing dominance of the smaller components of the benthic food webs. These data indicate that the sediments of the Rapallo Harbour were dominated by microbial biomasses to a larger extent than in non-food limited environments, characterized by a lower organic contamination. On the results presented in this study, the microbial dominance in highly organic enriched sediments can be explained with: (1) a reduction of the top-down control and grazing pressure of meio- and macrofauna on the microbial components; (2) the opportunistic composition and high metabolic activity of the microbial components.     

Changes in morphology and growth of the mudskipper (Periophthalmus argentilineatus) associated with coastal pollution

In this paper a comparison is made between the growth and morphology of barred mudskippers (Periophthalmus argentilineatus) from six mangrove forests along the coast of Tanzania. The fish populations from unpolluted sites consisted of different size classes, whereas only small sized fish were present in the polluted Mtoni mangroves. Age estimation based on the examination of otoliths revealed that the mudskippers followed similar growth patterns in all sites with limited pollution. However, the age estimates from the polluted Mtoni site revealed an abnormal growth pattern. The occurrence of unilateral anophthalmia in the Mtoni mudskippers suggested that these fish were affected by pollutants during early development. The study showed that the presence of urban and industrial wastes from Dar es Salaam city, as indicated by isotopic enrichment, correlated with abnormal growth and developmental effects in mudskippers. We hypothesize that pollution might also affect fish species that use the mangroves as a temporary habitat.     

Benthic Response to Mucilaginous Aggregates in the Northern Adriatic Sea: Biochemical Indicators of Eutrophication

In summer 1997, gelatinous aggregates appeared in the Adriatic Sea, covering large areas of the northern basin. This study deals with the comparison between the biochemical composition of the sedimentary organic matter in summer, 1996 (when no aggregates appeared), and in summer, 1997 (during the appearance of aggregates). the biochemical composition of organic matter in surface sediments (determined in terms of proteins, carbohydrates, lipids, phytopigments and nucleic acids) has been investigated in two areas along the coast of the NW-Adriatic Sea in order to characterize benthic processes during aggregate deposition on the sea floor. During mucilage accumulation, a significant increase of biochemical compounds was observed, and chlorophyll-a and carbohydrate concentrations doubled their concentrations. in contrast, protein concentrations decreased, so that overall biopolymeric carbon content (expressed as the sum of lipid, protein and carbohydrate carbon equivalents) did not display significant differences between sampling periods (1579.3 in June, 1996 1678.8 μgCg^-1 and June, 1997). the protein to carbohydrate ratio decreased from 4.9 in June, 1996 to 1.8 in June, 1997. Mucilage production in June, 1997, modified significantly the biochemical composition of the sedimentary OM, thus affecting the potential availability of OM to benthic consumers. We hypothesise that the production of highly refractory composition of the sedimentary OM during mucilage accumulation might have an important biogeochemical implications.     

Differentiation of protoplasm in nummulitidae (Foraminifera) from Elat,Red Sea

Chambers and canal system in the shells of Operculina ammonoides (Gronovius) and Heterostegina depressa d'Orbigny contain different protoplasm. The connections between the two main parts of the protoplasmic body are much smaller than the connections from chamber to chamber by the stolo system. The connections between chamber and canal system are located in the marginal sulcus and at the base of the chamber. The chamber protoplast (including the stolo system) is protected by a relatively thick, lamellar, mucopolysaccharide membrane — called organic lining — which represents also the template for the mineralization of the shell. Together, organic lining and shell form the cell wall. Over the pore holes in the lateral chamber walls, the organic lining thins out, but is not perforated. The plasma membrane below the organic lining seems to be differentiated by a bossy surface with comparatively coarse granules. The symbionts are concentrated below the lateral wall of the chambers, nestling against 2 or 3 pore-hole depressions. The differentiation of the organic lining, the plasma membrane below the pore holes, and the position of the symbionts in the chamber plasma point to a physiologic relationship between pores and symbionts. The cell organelles in the chamber protoplasm indicate the mainly metabolic function of the chamber protoplast. The protoplasm in the canal system is covered only by the plasma membrane, and is particularly rich in microtubuli similar to ordinary foraminiferal rhizopods. The canal system is, therefore, interpreted as consisting of a system of invaginations of the cell wall determining the morphology of proximal parts of the pseudopods.     

Benthic Response to Mucilaginous Aggregates in the Northern Adriatic Sea: Biochemical Indicators of Eutrophication

Abstract

In summer 1997, gelatinous aggregates appeared in the Adriatic Sea, covering large areas of the northern basin. This study deals with the comparison between the biochemical composition of the sedimentary organic matter in summer, 1996 (when no aggregates appeared), and in summer, 1997 (during the appearance of aggregates). the biochemical composition of organic matter in surface sediments (determined in terms of proteins, carbohydrates, lipids, phytopigments and nucleic acids) has been investigated in two areas along the coast of the NW-Adriatic Sea in order to characterize benthic processes during aggregate deposition on the sea floor. During mucilage accumulation, a significant increase of biochemical compounds was observed, and chlorophyll-a and carbohydrate concentrations doubled their concentrations. in contrast, protein concentrations decreased, so that overall biopolymeric carbon content (expressed as the sum of lipid, protein and carbohydrate carbon equivalents) did not display significant differences between sampling periods (1579.3 in June, 1996 1678.8 μgCg^?1 and June, 1997). the protein to carbohydrate ratio decreased from 4.9 in June, 1996 to 1.8 in June, 1997. Mucilage production in June, 1997, modified significantly the biochemical composition of the sedimentary OM, thus affecting the potential availability of OM to benthic consumers. We hypothesise that the production of highly refractory composition of the sedimentary OM during mucilage accumulation might have an important biogeochemical implications.     

Burrow morphology,biometry, age and growth of piddocks (Mollusca: Bivalvia: Pholadidae) on the south coast of England

Biometry and growth of three piddock species Pholas dactylus, Barnea candida and B. parva, from chalk and clay substrata were investigated between 1999 and 2000 at five low shore locations along the south coast of England. Piddock burrow shape was significantly different (P<0.01) amongst the locations. Burrows at Lyme Regis showed the largest (height/maximum diameter) ratio (4.86±2.00) whilst those at Compton the lowest (3.73±1.62). Using the method of Bhattacharya, the population structure of P. dactylus, B. candida and B. parva was separated into eight, three and five modal size classes, respectively. Age and shell growth were determined from the number and spacing, respectively, of annual growth lines present in acetate peel replicas of shell sections. The von Bertalanffy growth (VBG) equation fitted the size at age data obtained for P. dactylus and B. candida (L and K were 79.3±13.8 mm and 0.0011±0.22 and 29.6±1.5 mm and 1.17±0.47, respectively) whilst the size at age data for B. parva were linearly related and did not fit the assumptions of the VBG equation. Male and female gonads were mature and piddocks competent to spawn between June and September 1999, with settlement of juveniles observed between November 1999 and February 2000. A significant relationship between burrow aperture diameter and age of the occupant piddock was established for the three species. Burrow morphology and spatial distribution of burrows were influenced by substratum hardness and population density. Based on estimates at Lyme Regis, piddocks are capable of removing up to 41% of the shore substratum to a depth of 85 mm over their lifespan (12 years), significantly compromising the structural stability of the soft rock shores they inhabit and contributing to bioerosion.Communicated by O. Kinne, Oldendorf/Luhe     

沉积物中五氯酚对底栖生物的急慢性毒性效应

以淡水底栖动物花翅羽摇蚊幼虫和淡水单孔蚓为研究对象,研究了沉积物中五氯酚对底栖生物的急慢性毒性效应。五氯酚对花翅羽摇蚊幼虫96 h及10 d的半数致死浓度(LC50)分别为20.6 mg·kg-1和12.5 mg·kg-1,28 d羽化半数抑制浓度(EC50)为0.79 mg·kg-1。沉积物中五氯酚对花翅羽摇蚊幼虫的羽化具有延滞作用,而且对雌性摇蚊羽化的延滞作用大于雄性,最终导致羽化摇蚊的性别失衡。淡水单孔蚓对五氯酚的耐受力较摇蚊幼虫强。五氯酚对淡水单孔蚓的96 h及14 d的LC50分别为37.6 mg·kg-1和20.2 mg·kg-1,对淡水单孔蚓21 d生长抑制的EC50为1.39 mg·kg-1。研究结果对推导五氯酚沉积物质量基准和进行沉积物生态风险评价提供依据。     

Variability of shell growth and morphology of the wall-plate junctions of the intertidal barnacle Tesseropora rosea (Cirripedia: Tetraclitidae)

Variability in shell growth and morphology of the wallplate junctions of Tesseropora rosea (Krauss) were studied in 1983 in New South Wales, Australia, at two sites with differing wave exposure. The wall-plate junctions, a combination of dado (geometrically interlocking) and lap bints, increase in complexity with age, but do not differ between sites. The number of parietal tubes is fixed at settlement and does not differ between sites, but differs among wall plates in a manner consistent with their evolutionary history (rostrum > laterals > carina). The number of secondary septa increases with age, but does not differ between sites. In epilithic T. rosea, growth of the alae contributes to orifice enlargement. Epizoic T. rosea (on limpets) have conspicuous radii and display diametric growth. At the more exposed site, the shell wall was sleeper, and the aperture length, height and weight of the shell increased at a faster rate than at the less exposed site, but the maximum height of the shell was less. These differences appear to be due to a combination of greater feeding rates and greater erosion rates at the exposed site. The greater maximum height attained at the more sheltered site may be due to greater individual longevity. Juveniles at the sheltered site had thinner septa in the laterals than those at the exposed site. Septa in adults were rhinner at the exposed site, but this is due to age differences between sites in the adult populations.