Alan T. Marshall

Low temperature FESEM of the calcifying interface of a scleractinian coral

The ultrastructural nature of the calcifying interface in the scleractinian coral Galaxea fascicularis has been investigated using high-resolution, low temperature field emission scanning electron microscopy (FESEM). This technique permitted structural analyses of soft tissue and skeleton in G. fascicularis in a frozen-hydrated state, without the need for chemical fixation or decalcification. Structural comparisons are made between frozen-hydrated polyps and polyps that have undergone conventional fixation and decalcification. Vesicles expelled by the calicoblastic ectodermal cells into sub-skeletal spaces and previously suggested to play a role in calcification were commonly observed in fixed samples but were distinctly absent in frozen-hydrated preparations. We propose that these vesicles are fixation artefacts. Two distinct types of vesicles (380 and 70 nm in diameter, respectively), were predominant throughout the calicoblastic ectodermal cells of frozen-hydrated preparations, but these were never seen to be entering, or to be contained within, sub-skeletal spaces, nor did they contain any crystalline material. In frozen-hydrated preparations, membranous sheets were seen to surround and isolate portions of aboral mesogloea and to form junctional complexes with calicoblastic cells. The calicoblastic ectoderm was closely associated with the underlying skeleton, with sub-skeletal spaces significantly smaller (P<0.0001) in frozen-hydrated polyps compared to fixed polyps. A network of organic filaments (26 nm in diameter) extended from the apical membranes of calicoblastic cells into these small sub-skeletal cavities. A thin sheath was also frequently observed adjacent to the apical membrane of calicoblastic cells.

Temperature effects on calcification rate and skeletal deposition in the temperate coral, Plesiastrea versipora (Lamarck)

Abstract The geographic range of the coral, Plesiastrea versipora (Lamarck, 1816), extends into temperate waters outside the southern limit for hermatypic corals. In the present study, calcification in Plesiastrea collected from Port Phillip Bay, Victoria was examined over the corals normal annual temperature range (10–21 °C), which is well below the normal optimum for coral calcification in tropical corals (25–28 °C). Calcification rate in Plesiastrea was considerably lower than in reef corals, but showed a similar pattern in temperature responses, with a trend towards higher rates at ∼18 °C. The light/dark calcification ratio was markedly lower than that in tropical corals. Autoradiography showed that calcification occurred primarily by deposition of calcium carbonate at the upper surfaces of the septo-costae. Scanning electron microscopy (SEM) showed that skeletal deposition in Plesiastrea had a temperature-dependent diel pattern. In the light, calcium carbonate was deposited as small spheroidal crystals and, at higher temperatures, small needle-shaped crystals. In the dark, calcium carbonate deposition appeared to be in the form of an amorphous sheet-like cementation. Compared with other scleractinian corals, calcification rate in Plesiastrea was relatively slow and showed different patterns of skeletal deposition.

Three-dimensional localization of CENP-A suggests a complex higher order structure of centromeric chromatin

The histone H3 variant centromere protein A (CENP-A) is central to centromere formation throughout eukaryotes. A long-standing question in centromere biology has been the organization of CENP-A at the centromere and its implications for the structure of centromeric chromatin. In this study, we describe the three-dimensional localization of CENP-A at the inner kinetochore plate through serial-section transmission electron microscopy of human mitotic chromosomes. At the kinetochores of normal centromeres and at a neocentromere, CENP-A occupies a compact domain at the inner kinetochore plate, stretching across two thirds of the length of the constriction but encompassing only one third of the constriction width and height. Within this domain, evidence of substructure is apparent. Combined with previous chromatin immunoprecipitation results (Saffery, R., H. Sumer, S. Hassan, L.H. Wong, J.M. Craig, K. Todokoro, M. Anderson, A. Stafford, and K.H.A. Choo. 2003. Mol. Cell. 12:509–516; Chueh, A.C., L.H. Wong, N. Wong, and K.H.A. Choo. 2005. Hum. Mol. Genet. 14:85–93), our data suggest that centromeric chromatin is arranged in a coiled 30-nm fiber that is itself coiled or folded to form a higher order structure.

Calcium associated with a fibrillar organic matrix in the scleractinian coral Galaxea fascicularis

Summary. Field emission scanning electron microscopy of frozen-hydrated preparations of the scleractinian coral Galaxea fascicularis revealed organic fibrils which have a diameter of 26 nm and are located between calicoblastic ectodermal cells and the underlying CaCO3 skeleton. Small (37 nm in diameter) nodular structures observed upon this fibrillar organic material possibly correspond to localised Ca-rich regions detected throughout the calcifying interfacial region of freeze-substituted preparations by X-ray microanalysis. We propose that these Ca-rich regions associated with the organic material are nascent crystals of CaCO3. Significant amounts of S were also detected throughout the calcifying interfacial region, further verifying the likely presence of organic material. However, the bulk of this S is unlikely to be derived from mucocytes within the calicoblastic ectoderm. It is suggested that in the scleractinian coral G. fascicularis, nodular crystals of CaCO3 establish upon a fibrillar, S-containing, organic matrix within small but distinct extracellular pockets formed between calicoblastic ectodermal cells and skeleton. This arrangement conforms with the criteria necessary for biomineralisation and with the long-held theory that organic matrices may act as templates for crystal formation and growth in biological mineralising systems.

Studies on water and ion transport in homopteran insects: ultrastructure and cytochemistry of the cicadoid and cercopoid Malpighian tubules and filter chamber.

Abstract The filter chamber is a complex junction of anterior and posterior extremities of the midgut and Malpighian tubules. The sac-like anterior extremity, or filter chamber proper, comprises two cell types. These are large cuboidal cells which secrete a mucoprotein, and extremely thin cells which have regular tubular invaginations of the basal plasma membrane. The posterior extremity of the midgut and the internal Malpighian tubules coil round the filter chamber proper. They consist of thin epithelial cells identical in ultrastructure. The basal plasma membrane in these cells is formed into leaflets. A thin cellular sheath and thick muscle layers surround the filter chamber. The filter chamber proper is lined by the mucoprotein secretion of the cuboidal cells. This secretion appears to bind potassium ions. ATPase and alkaline phosphatase cannot be detected in the filter chamber epithelia. The structure and cytochemistry of the filter chamber suggests that water flows from filter chamber proper to midgut and Malpighian tubules by passive osmosis. This may be facilitated by ion binding in the filter chamber proper and by hydrostatic pressure engendered by contraction of the muscular coat. The Malpighian tubules appear to be structurally and chemically adapted for ion secretion by active transport and possibly for reabsorption in the Malpighian duct segment.

Electron and ion microprobe analysis of calcium distribution and transport in coral tissues

SUMMARY It is shown by x-ray microanalysis that a gradient of total intracellular Ca concentration exists from the outer oral ectoderm to the inner skeletogenic calicoblastic ectoderm in the coral Galaxea fascicularis. This suggests an increase in intracellular Ca stores in relation to calcification. Furthermore, Ca concentration in the fluid-filled space of the extrathecal coelenteron is approximately twice as high as in the surrounding seawater and higher than in the mucus-containing seawater layer on the exterior of the oral ectoderm. This is indicative of active Ca2+ transport across the oral epithelium. Polyps were incubated in artificial seawater in which all 40Ca was replaced by 44Ca. Imaging Ca2+ transport across the epithelia by secondary ion mass spectroscopy (SIMS) using 44Ca as a tracer showed that Ca2+ rapidly entered the cells of the oral epithelium and that 44Ca reached higher concentrations in the mesogloea and extrathecal coelenteron than in the external seawater layer. Very little Ca2+ was exchanged in the mucocytes, cnidocytes or zooxanthellae. These observations again suggest that Ca2+ transport is active and transcellular and also indicate a hitherto unsuspected role in Ca2+ transport for the mesogloea.

Skeletal Microstructure of Galaxea fascicularis Exsert Septa: A High-Resolution SEM Study

The deposition of four crystal types at the growth surface of the septa of several color morphs of the coral Galaxea fascicularis was investigated over a 24-h period. Results suggest that nanocrystals, on denticles at the apices of exsert septa, may be the surface manifestation of centers of calcification. These crystals were also found on the septa of the axial corallite of Acropora formosa. The deposition of nanocrystals appears to be independent of diurnal rhythms. Internally and proximal to the septal apices, distinct clusters of polycrystalline fibers originate from centers of calcification and form fanlike fascicles. Upon these fascicles, acicular crystals grow and extend to form the visible fasciculi at the skeletal surface. Deposition of aragonitic fusiform crystals in both G. fascicularis and A. formosa occurs without diurnal rhythm. Nucleation of fusiform crystals appears to be independent of centers of calcification and may occur by secondary nucleation. Formation of semi-solid masses by fusiform crystals suggests that the crystals may play a structural role in septal extension. Lamellar crystals, which have not been reported as a component of scleractinian coral skeletons before, possess distinct layers of polyhedral plates, although these layers also do not appear to be associated with daily growth increments. The relationship of lamellar crystals to other components of the scleractinian coral skeleton and their involvement in skeletal growth is unknown.

Light-regulated Ca2+ uptake and O2 secretion at the surface of a scleractinian coral Galaxea fascicularis.

The surface concentration dynamics of Ca(2+) and O(2) in the scleractinian coral Galaxea fascicularis were investigated by means of 2 mm-sized sensors (mini-electrodes). Mini-electrodes were used to measure the light-regulated uptake of Ca(2+) for calcification, and the secretion of O(2), produced by photosynthesising zooxanthellae, at the surface of the oral ectoderm of Galaxea polyps. The concentration of Ca(2+) measured in the boundary layer of seawater adjacent to the polyp surface was variable but always higher than in bulk seawater in the dark and fell to levels closer to the value in bulk seawater on illumination. The fall in concentration, representing an influx of Ca(2+) into the ectoderm, increased with increasing photosynthetic photon flux density of illumination. The decrease in Ca(2+) concentration on illumination was insensitive to ruthenium red but sensitive to verapamil and acetazolamide. Oxygen secretion at the ectoderm, manifested by an increase in O(2) concentration in the boundary layer, increased on illumination but was not sensitive to any of the inhibitors used in the calcium experiments. The results suggest that Ca(2+) uptake involves calcium channels and is coupled in someway to the uptake of inorganic carbon for calcification. Uptake is also strongly coupled to photosynthesis.

Ultrastructure changes associated with osmoregulation in the hindgut cells of a saltwater insect, Ephydrella SP. (Ephydridae: Diptera)

Abstract Ephydrella larvae strictly regulate their blood osmotic pressure and Na + content over a wide range of environmental salinities (7 mM to 3000 mM NaCl). They can survive in distilled water and 6000 mM NaCl for several days. In the hindgut the ileum is concerned with the regulation of urine composition whilst the rectum has a purely mechanical function. In the ileum there are large cells which have long basal channels and short apical microvilli, and small cells which have long apical leaflets and short basal channels. It is suggested that the large cells reabsorb water and that the small cells either reabsorb or secrete ions. The configurations of the channels, and the spacing of leaflets and microvilli change with alterations in environmental salinity. Fixation experiments using fixatives of different osmotic pressures show that the configuration of extracellular space in the cells has a marked dependence on both the osmotic pressure of the fixative and upon the environmental salinity. It is suggested that the osmotic response of the cells to fixatives indicates that the osmotic pressure of the cells increases with increasing environmental salinity. It is suggested, in general, that correlation of changes in the volume of extracellular space with changes in ion and water transport must be regarded with caution.

Thermal compensation of metabolism in the temperate coral, Plesiastrea versipora (Lamarck, 1816)

Plesiastrea versipora is a hermatypic coral with a distribution that extends to the southern limit for hermatypic corals. The normal annual temperature range for this coral in Port Phillip Bay (Victoria) (approximately 10-21 degrees C) is well below the physiological optimum for the majority of hermatypic corals (25-29 degrees C). The rate of photosynthesis and respiration in Plesiastrea generally increased with temperature before levelling out at the higher temperatures, with Q(10) data suggesting that both photosynthesis and respiration in Plesiastrea acclimate to changing temperatures. Respiration showed a similar trend to photosynthesis, with respect to temperature, but with a slightly lower rate of increase. Photosynthetic rate in Plesiastrea is comparable with that of reef corals despite lower temperatures and irradiance. When expressed as a function of chlorophyll a content photosynthesis approached perfect temperature compensation with prolonged exposure to various temperatures. Temperature-dependent changes with chlorophyll content may be responsible for temperature related changes in photosynthetic rate. This may be a mechanism for stabilising the symbiotic relationship over a wide temperature range. Autotrophic ability, estimated from photosynthesis/respiration (P/R) ratios, was greatest at higher temperatures and was only slightly less than that of reef corals. At low temperatures Plesiastrea may be dependent on heterotrophic feeding.