Cellular defense reactions of the shore crab, Carcinus maenas: in vivo hemocytic and histopathological responses to injected bacteria

The cellular defense reactions of the shore crab, Carcinus maenas, were studied, following injections of the bacteria Bacillus cereus and Moraxella sp., by histological and ultrastructural examination of the gills, heart, and hepatopancreas. The majority of the bacteria were sequestered to the gills, but some were also later evident in the heart and hepatopancreas. The presence of the bacteria in the gills initiated the formation of numerous small cell clumps, composed of both refractile and phagocytic cells, which entrapped many microorganisms. The clumps reached a maximum size 6 hr after inoculation and although some were cleared from the gills others persisted for 7 days, becoming more compact and necrotic during this period. Clump formation appears to occur following recognition of the bacteria as foreign and results in the hemocytes becoming sticky and adherent. The response is very effective in rapidly immobilizing the bacteria, thus restraining the spread of infection. It is proposed that this phenomenon may be a significant component of crustacean cellular host defenses.     

Analysis of actin and microfilament-associated proteins in the mitotic spindle and cleavage furrow of PtK2 cells by immunofluorescence microscopy: A critical note

The distribution of actin and the microfilament-associated proteins myosin and tropomyosin was studied in mitotic PtK2 cells. Using fluorescent heavy meromyosin and two different antibodies against actin we have found no evidence for increased accumulations of actin in the mitotic spindle but have found increased levels of actin in the cleavage furrow and the contractile ring. Short, thin microfilament pieces remain detectable in the cytoplasm throughout mitosis. Purified antibodies against myosin and tropomyosin also revealed no increased levels of these proteins in the spindle region, although both proteins were found in the contractile ring and areas of the cytoplasm close to the intercellular bridge. These data are in agreement with functional and ultrastructural studies involving a role for actin and microfilament-related proteins in cytokinesis. They do not support models in which microfilament-related proteins are assumed to be a major constituent of the mitotic spindle.     

On functional morphology of the skeleton in lychnisc sponges (Porifera,Hexactinellida)

By comparison with architectural models it can be shown that both the “euretoid” arrangement of fused spicules and lychnisc node itself should enhance the strength of the skeleton of the Lychniscosa. Contrary to expectation however, the Lychniscosa do not inhabit more turbulent waters than the Hexactinosa with a simpler skeletal structure. Possible reasons for this are discussed.     

An organ culture system for study of fetal lung development

Fetal rat lungs placed in $\text{in}$$\text{vitro}$ organ culture at 15.5 days gestation grow significantly based on accumulation of DNA and protein. In the experimental system described, DNA accumulated rapidly during the first three days in culture and increased from 4.8 to 15.6 micrograms per lung culture. Protein content increased more slowly and reached a value more than double the initial value after six days in the culture system. Glycogen accumulated in the tissue during the first six days in culture and was depleted during the subsequent culture period, a pattern strikingly similar to that observed during lung development $\text{in}$$\text{vivo}$. Phospholipid accumulation was biphasic with respect to time with an inflection point at about the sixth day of culture. The phosphatidylcholine species synthesized in the culture system $\text{in}$$\text{vitro}$ were similar to those produced $\text{in}$$\text{vivo}$ in fetal lung at 21 days gestation.     

Lysyl oxidase dependent synthesis of a collagen cross-link containing histidine

To date, collagen appears unique among proteins in that it contains histidine in certain of its cross-links. Synthesis of histidine containing collagen cross-links was studied in vitro with lathyritic L-¹⁴C histidine or L-¹⁴C lysine labelled bone collagen fibrils and purified lysyl oxidase. Synthesis of the tetrafunctional cross-link, dehydrohistidinohydroxymerodesmosine occurred with lysyl oxidase and was inhibited by β-aminopropionitrile. Synthesis began after a lag period of sixteen hours and then proceeded linearly for four days. These data indicate that enzyme dependent synthesis of dehydrohistidinohydroxymerodesmosine occurs in vitro in a biochemically defined system. Biosynthesis in vivo might occur under similar conditions.     

A 25,000 molecular weight protein constituent of human amyloid fibrils related to amyloid protein AA

Amyloid fibrils from a patient with diffuse amyloid disease are dissociated in 6 m guanidine hydrochloride and fractionated by gel chromatography. Two major components are separated on Sepharose 6B. Both proteins are characterized by chromatography, immunodiffusion, discontinuous gel electrophoresis, amino acid tryptic peptide mapping and amino acid sequence analysis. The smaller of the two components is typical of the known protein AA by size (8400 daltons), amino acid composition and a 30-residue N-terminal sequence. The larger of the components (25,000 daltons) undergoes electrophoresis as a single band and appears unaffected by thiol reduction. It differs from protein AA in amino acid content and by its tryptic peptide map, although it contains an N-terminal amino acid sequence identical to protein AA when carried to 20 residues. Treatment of this larger component by mild acid hydrolysis results in the release of the 8400-dalton protein AA. Fractionation after guanidine hydrochloride treatment of this particular amyloid fibril preparation is compared to the fractionation of a typical secondary amyloid preparation that contains only protein AA as the major component. The origin and relationship of the 8,400- and 25,000-dalton protein components is discussed.     

Paleocene benthonic foraminiferal biostratigraphy,paleobiogeography and paleoecology of Atlantic—Tethyan regions: Midway-type fauna

The stratigraphic, geographic and bathymetric distribution of some Paleocene benthonic foraminiferal assemblages have been studied in the Tethyan and circum-Atlantic regions within the framework of planktonic foraminiferal zones. Although some species appear to be restricted to either the Tethyan-European area or to the western Atlantic, the majority of species are amphi-Atlantic and Tethyan in distribution. The cosmopolitan distribution is attributed to more equitable climatic conditions (lower polar—equatorial thermal gradient) and warmer, more uniform thermal structure of the oceans and different paleogeographic and paleo-oceanographic conditions.Two main distinct depth-controlled benthonic foraminiferal assemblages (exclusive of the shallow-warm water Tethyan carbonate assemblage) have been recognized in the Paleocene. The continental shelf fauna, termed here the “Midway-type fauna” (MF) is characterized by species of Cibicidoides alleni (Plummer) = propria Brotzen, howelli (Toulmin), succedens (Brotzen), Anomalinoides [acuta (Plummer), midwayensis (Plummer)], Gavelinella [danica (Brotzen), neelyi (Jennings)], and Osangularia plummerae Brotzen, as well as various lagenids (nodosariids, lenticulinids, vaginulinids), polymorphinids and textulariids. A lower continental slope and abyssal plain fauna, termed here the “Velasco-type fauna” (VF), is characterized by, amongst others, Gavalinella [beccariiformis (White), rubiginosa (Cushman), velascoensis (Cushman)], Nuttallides truempy (Nuttall), Nuttallinella florealis (Cushman), velascoensisZ (Cushman)], (Cushman), Aragonia velascoensis (Cushman), nodosariids (N. velascoensis Cushman, Dentalina limbata d'Orbigny), various agglutinated forms [Gaudryina pyramidata Cushman, Tritaxia aspera (Cushman), Dorothia ex. gr. oxycona trinitatensis (Cushman and Renz)], and various gyroidinids and buliminids. Pleuriostomellids and stilostomellids are quantitatively rare and unimportant until the Middle—Late Eocene.This paper discusses the biostratigraphy and biogeography of the “Midway-type fauna”.