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101.
Prof. Dr. Gerd Flajs Dipl.-Geol. Manfred Vigener Prof. Dr. Helmut Keupp Prof. Dr. Dieter Meischner Dipl.-Geol. Fritz Neuweiler PD Dr. Josef Paul Prof. Dr. Joachim Reitner Dr. Klaus Warnke PD Dr. Helmut Weller Dipl.-Geol. Patrick Dingle Dipl.-Geol. Christian Hensen Prof. Dr. Priska Schäfer Dr. Pascale Gautret Prof. Dr. Reinhold R. Leinfelder PD Dr. Hansmartin Hüssner Dipl.-Geol. Bernd Kaufmann 《Facies》1995,32(1):1-69
Summary This research report contains nine case studies (part II to X) dealing with Palaeozoic and Mesozoic mud mounds, microbial
reefs, and modern zones of active micrite production, and two parts (I and XI) summarizing the major questions and results.
The formation of different types ofin situ formed micrites (automicrites) in close association with siliceous sponges is documented in Devonian, Carboniferous, Triassic,
Jurassic and Cretaceous mounds and suggests a common origin with a modern facies found within reef caves. Processes involved
in the formation of autochthonous micrites comprise: (i) calcifying mucus enriched in Asp and Glu, this type presumably is
linked to the formation of stromatolites, thrombolites and massive fabrics; (ii) protein-rich substances within confined spaces
(e.g. microcavities) result in peloidal pockets, peloidal coatings and peloidal stromatolites, and (iii) decay of sponge soft
tissues, presumably enriched with symbiotic bacteria, lead to the micropeloidal preservation of parts of former sponge bodies.
As a consequence, there is strong evidence that the primary production of micrite in place represents the initial cause for
buildup development. The mode of precipitation corresponds to biologically-induced, matrix-mediated mineralization which results
in high-Mg-calcites, isotopically balanced with inorganic cements or equilibrium skeletal carbonates, respectively. If distinct
automicritic fabrics are absent, the source or origin of micrite remains questionable. However, the co-occurring identifiable
components are inadequate, by quantity and physiology, to explain the enhanced accumulation of fine-grained calcium carbonate.
The stromatolite reefs from the Permian Zechstein Basin are regarded as reminiscent of ancestral (Precambrian) reef facies,
considered the precursor of automicrite/sponge buildups. Automicrite/sponge buildups represent the basic Phanerozoic reef
type. Analogous facies are still present within modern cryptic reef habitats, where the biocalcifying carbonate factory is
restricted in space. 相似文献
102.
Evolutionary relationships among the male and female mitochondrial DNA lineages in the Mytilus edulis species complex 总被引:1,自引:0,他引:1
A novel form of mitochondrial DNA (mtDNA) inheritance has previously been
documented for the blue mussel (Mytilus edulis). Female mussels inherit
their mtDNA solely from their mother while males inherit mtDNA from both
their mother and their father. In males, the paternal mtDNA is
preferentially amplified so that the male gonad is highly enriched for the
paternal mtDNA that is then transmitted from fathers to sons. We
demonstrate that this mode of mtDNA inheritance also operates in the
closely related species M. galloprovincialis and M. trossulus. The
evolutionary relationship between the male and female mtDNA lineages is
estimated by phylogenetic analysis of 455 nucleotides from the large
subunit ribosomal RNA gene. We have found that the male and female lineages
are highly divergent; the divergence of these lineages began prior to the
speciation of the three species of blue mussels. Further, the separation
between the male and female lineages is estimated to have occurred between
5.3 and 5.7 MYA.
相似文献
103.
PD Dr. Hartmut Greven 《Cell and tissue research》1980,212(1):147-162
Summary The uterine epithelium of pregnant females of the terrestrial ovoviviparous Salamandra salamandra is characterized by a considerable enlargement of its basolateral surface. Chloride and cations (among others sodium), preferentially within the intercellular spaces, can be demonstrated ultrahistochemically. There is indirect evidence of Na+-K+-ATPase activity along the basolateral plasma membranes of the epithelial cells using the Sr-technique for demonstration of a K+-NPPase and 3H-ouabain autoradiography. Preliminary measurements reveal a potential difference across the uterine wall of 15–25mV, the lumenal (mucosal) surface being negative with respect to the coelomic (serosal) surface, and a short circuit current of 200–300 A. The possibly electrogenic ion transport is ouabain-sensitive. The results are in agreement with the model of a forward transporting, i.e. absorptive epithelium. An active transport of solute out of the uterine lumen across the epithelium to the subjacent connective tissue and the blood vessels may be involved in the regulation of an intrauterine milieu appropriate for the development of the offspring.I am indebted to Miss Dr. U. Beigel, Zoologisches Institut der Universität Münster, for linguistic help 相似文献
104.
Diethylcarbamazine (DEC) was active in vitro against infective larvae and microfilariae of Brugia pahangi but only at high concentrations. When fed to mosquitoes which were infected with B. pahangi it had little or no activity. In jirds it was inactive against B. pahangi microfilariae and adults when administered at 300 mg/kg for 5 days either by the intraperitoneal or oral route. In cats given 25 or 50 mg DEC/kg intraperitoneally on 3 or 5 occasions it was not microfilaricidal, but most of the adult worms died within 30 days of the end of treatment. Although most microfilariae disappeared from the blood of cats immediately (i.e., within an hour) after treatment, they reappeared within a few hours in the same numbers. Microfilarial levels were reduced after treatment but there was no precipitate decline as occurs in human B. malayi patients. 相似文献
105.
Recorded in several species including humans, geophagia or soil eating has been observed in both wild and domesticated horses and has generally been regarded as an indication of nutritional deficiency or "boredom". Studies of soils consumed by different species have led to several theories as to the identity of soil constituents that stimulate geophagia. In this study, geochemical analysis of 13 equine geophagic sites from different parts of Australia was undertaken. Significantly larger concentrations of iron and copper were found in soil samples from geophagic sites when compared to paired control samples, suggesting that these elements provide the stimulus for geophagia. 相似文献
106.
William F. Wood Jeffrey P. Copeland Richard E. Yates Iman K. Horsey Lynne R. McGreevy 《Biochemical Systematics and Ecology》2009
Urine deposition has been observed as an important scent-marking behaviour among wolverines (Gulo gulo, Mustelinae, Mustelidae). Solid phase microextraction (SPME) of headspace volatiles of the urine from free ranging wolverines were examined by gas chromatography–mass spectrometry (GC–MS). Urine samples were collected directly from the bladder of live-trapped animals or from frozen samples deposited in snow. Nineteen potential semiochemicals were identified in the headspace from 22 urine samples. The composition of these volatile compounds varied by type and amount with each sample, but a number of chemicals were regularly found in many samples. The most commonly found constituents were the ketones; 2-heptanone, 4-heptanone and 4-nonanone; and the terpenes: α-pinene, β-pinene, limonene, linalool and geraniol. Mammalian urinary discharge of ingested α-pinene, β-pinene, limonene and other hydrocarbon terpenes is unusual, as these compounds are usually oxidized before excretion. The source of the hydrocarbon monoterpenes likely includes conifer needles, as they have been found in wolverine scat. 相似文献
107.
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110.
The intact epicuticles of Strongyloides ratti stage-3 larvae and Trichinella spiralis stage-1 larvae were found to have a surface net negative charge. Ultrastructural studies on S. ratti using cationized ferritin and ruthenium red showed the negative charge to be dense and uniformly distributed over the epicuticular surface. Staining with acetic acid-ferric oxide hydrosol occurred at pH 1.65 and suggests that amino acid carboxyl groups were not responsible for the negative charge property. Alcian blue staining occurred at pH 0.5 and at a critical electrolyte concentration (CEC) of 0.9 M MgCl2, a property similar to that of highly sulfated mucopolysaccharides such as the proteoglycan keratan sulfate. In contrast, T. spiralis larvae failed to stain with alcian blue below pH 5.0 or at a CEC of 0.1 M, suggesting its negative charge is associated with dissociated amino acid carboxyl groups. Attempts to remove the negative charge-bearing components in the epicuticle of S. ratti by detergents, organic solvents, denaturing agents, proteases, uronidases, neuraminidases, and lipases were unsuccessful. The presence of elastin in the S. ratti larval outer cortical layer was indicated by its vulnerability to elastase and its reaction to aldehyde fuchsin-alcian blue stain. These results show that the epicuticle of S. ratti is not a typical cell membrane, although it appears to have ultrastructural similarities. It is suggested that the association of highly sulfated mucopolysaccharides with the epicuticular surface of free-living nematodes such as S. ratti L3 may reflect a greater need to protect against surface desiccation. It is also postulated that the highly negatively charged surface may have anticomplementary and anticoagulation effects. 相似文献