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Thin, pyroclastic marker beds are preserved in argillaceous units of the Dwyka Group in southern Nambia and South Africa which are the earliest witnesses of volcanism in Karoo-equivalent strata of southern Africa. The aim of this study is to present the field appearance of these marker beds, to characterise their mineralogy, geochemistry and heavy mineral contents and to present new radiometric age data from their juvenile zircons. Carboniferous-Permian Karoo deposits in the Aranos Basin of southern Namibia include the glacially dominated, Carboniferous Dwyka Group and the shelf sediments of the overlying Permian Ecca Group. The Dwyka Group can be subdivided into four upward-fining deglaciation sequences, each capped by relatively fine-grained glaciolacustrine or glaciomarine deposits. The uppermost part of the second deglaciation sequence comprises a thick fossiliferous mudstone unit, referred to as the ”Ganigobis Shale Member”. An abundance of marine macro- and ichnofossils as well as extrabasinally derived ashfall tuff beds characterise the more than 40 m thick mudstones and provide the basis for an integrated high-resolution biostratigraphic and tephrostratigraphic framework. The Ganigobis Shale Member contains remains of paleoniscoid fishes, bivalves, gastropods, scyphozoa, crinoid stalks, sponges and sponge spicules, radiolaria, coprolites and permineralised wood. These mostly marine body and trace fossils record the extent of the first of a series of marine incursions into the disintegrating Gondwanan interior as early as the Carboniferous. Within the Ganigobis Shale Member 21 bentonitic tuff beds displaying a thickness of 0.1 and 2.0 cm were determined which in part can be traced laterally over tens of kilometres indicating an ashfall derivation. Further bentonitic tuff beds of the Dwyka Group were detected in cut banks of the Orange River near Zwartbas in the Karasburg Basin (southern Namibia). The 65 tuff beds vary between 0.1 and 4.0 cm in thickness. Due to a similar fossil content and age of the background deposits, the tuff beds are thought to have originated from the same source area as those from the Aranos Basin. Thin-sections reveal the derivation of the tuff beds as distal fallout ashes produced by explosive volcanic eruptions. The matrix consists of a micro- to cryptocrystalline clay mineral-quartz mixture. Rare fragments of splinter quartz, completely recrystallized ash-sized particles of former volcanic glass and few apatite and zircon grains are the only juvenile components. The tuff beds contain as non-opaque, juvenile heavy minerals mostly zircon, apatite, monazite and sphene but also biotite, garnet, hornblende and tourmaline. Geochemical analyses point to an original, intermediate to acid composition of the tuff samples. LREE enrichment and Eu-anomalies show that the parent magma of the tuff beds was a highly evolved calc-alkaline magma. Tectonomagmatic discrimination diagrams point to a volcanic arc setting. Bedding characteristics and the lack of any Carboniferous-Permian volcanic successions onshore Namibia makes an aeolian transport of the ash particles over larger distances likely. Siliceous ashes could thus have been transported by prevailing south-westerly winds from arc-related vents in South America to southern Africa. A second, more local source area could have been located in an intracontinental rift zone along the western margin of southern Africa which is indicated by north-south directed ice-flow directions in the Late Carboniferous. SHRIMP-based age determinations of juvenile magmatic zircons separated from the tuff beds allow a new time calibration of Dwyka Group deglaciation sequences II - IV and the Dwyka/Ecca boundary. Zircons of the Ganigobis Shale Member yield SHRIMP-ages of 302-300 Ma. This dates the uppermost part of the second deglaciation sequence in southern Namibia to the Late Carboniferous (Gzelian) and provides a minimum age for the onset of Karoo-equivalent marine deposition. The age of the uppermost argillaceous part of the third deglaciation sequence (297 Ma) was determined from zircons of a tuffaceous bed sampled in a roadcut in the Western Cape Province, South Africa. The deposits correlate with the Hardap Shale Member in the Aranos Basin of southern Namibia which are part of much more widespread Eurydesma transgression. The age of the Dwyka/Ecca boundary was determined by SHRIMP-measurements of juvenile zircons from two tuff beds of the basal Prince Albert Formation sampled in the Western Cape Province (South Africa). The zircons revealed ages of 289 - 288 Ma which date the Dwyka/Ecca boundary at about 290 Ma. According to these ages, deglaciation sequences II-IV lasted for 5 Ma on average.
Most natural learning situations are of a complex nature and consist of a tight conjunction of the animal's behavior (B) with the perceived stimuli. According to the behavior of the animal in response to these stimuli, they are classified as being either biologically neutral (conditioned stimuli, CS) or important (unconditioned stimuli, US or reinforcer). A typical learning situation is thus identified by a three term contingency of B, CS and US. A functional characterization of the single associations during conditioning in such a three term contingency has so far hardly been possible. Therefore, the operational distinction between classical conditioning as a behavior-independent learning process (CS-US associations) and operant conditioning as essentially behavior-dependent learning (B-US associations) has proven very valuable. However, most learning experiments described so far have not been successful in fully separating operant from classical conditioning into single-association tasks. The Drosophila flight simulator in which the relevant behavior is a single motor variable (yaw torque), allows for the first time to completely separate the operant (B-US, B-CS) and the classical (CS-US) components of a complex learning situation and to examine their interactions. In this thesis the contributions of the single associations (CS-US, B-US and B-CS) to memory formation are studied. Moreover, for the first time a particularly prominent single association (CS-US) is characterized extensively in a three term contingency. A yoked control shows that classical (CS-US) pattern learning requires more training than operant pattern learning. Additionally, it can be demonstrated that an operantly trained stimulus can be successfully transferred from the behavior used during training to a new behavior in a subsequent test phase. This result shows unambiguously that during operant conditioning classical (CS-US) associations can be formed. In an extension to this insight, it emerges that such a classical association blocks the formation of an operant association, which would have been formed without the operant control of the learned stimuli. Instead the operant component seems to develop less markedly and is probably merged into a complex three-way association. This three-way association could either be implemented as a sequential B-CS-US or as a hierarchical (B-CS)-US association. The comparison of a simple classical (CS-US) with a composite operant (B, CS and US) learning situation and of a simple operant (B-US) with another composite operant (B, CS and US) learning situation, suggests a hierarchy of predictors of reinforcement. Operant behavior occurring during composite operant conditioning is hardly conditioned at all. The associability of classical stimuli that bear no relation to the behavior of the animal is of an intermediate value, as is operant behavior alone. Stimuli that are controlled by operant behavior accrue associative strength most easily. If several stimuli are available as potential predictors, again the question arises which CS-US associations are formed? A number of different studies in vertebrates yielded amazingly congruent results. These results inspired to examine and compare the properties of the CS-US association in a complex learning situation at the flight simulator with these vertebrate results. It is shown for the first time that Drosophila can learn compound stimuli and recall the individual components independently and in similar proportions. The attempt to obtain second-order conditioning with these stimuli, yielded a relatively small effect. In comparison with vertebrate data, blocking and sensory preconditioning experiments produced conforming as well as dissenting results. While no blocking could be found, a sound sensory preconditioning effect was obtained. Possible reasons for the failure to find blocking are discussed and further experiments are suggested. The sensory preconditioning effect found in this study is revealed using simultaneous stimulus presentation and depends on the amount of preconditioning. It is argued that this effect is a case of 'incidental learning', where two stimuli are associated without the need of reinforcement. Finally, the implications of the results obtained in this study for the general understanding of memory formation in complex learning situations are discussed.
Previous work on Jurassic bivalves from the Iberian Range is reviewed, whereby emphasis is placed on Callovian-Kimmeridgian species. The taxonomy, distribution pattern and ecology of the bivalve fauna occurring in Middle and Upper Jurassic rocks of the Aragonian Branch of the Iberian Range have been analysed. For this purpose 14 sections and 5 additional outcrops, selected according to the abundance of bivalves, were measured in detail and sampled. The rocks studied belong to the Chelva, Yátova, Sot de Chera and Loriguilla formations of Callovian-Kimmeridgian age. The distribution of species of bivalves is given for each section. More than 3000 specimens of bivalves representing 83 species that belong to 46 genera and subgenera of the subclasses Palaeotaxodonta, Pteriomorphia, Isofilibranchia. Palaeoheterodonta, Heterodonta and Anomaldesmata have been used for the taxonomic analysis. One species is new: Plagiostoma fuersichi from the Callovian of the Chelva Fm. The autecology (trophic group and life habit) of each bivalve has been discussed. 49 samples of four sections habe been selected for a quantitative palaeoecological analysis of the bivalve fraction of the benthic fauna. Five bivalve associations and two assemblages are recognised by a Q-mode hierarchical cluster analysis (Ward method). The main environmental factors controlling bivalve associations are thought to be substrate, water energy and distribution of organic matter. The bivalves exhibit a distinct spatial and temporal distribution pattern within the Aragonian Branch. Four of the bivalve associations occur in the Upper Oxfordian (Sot de Chera Fm) and one association in the Lower Callovian (Chelva Fm). In the Sot de Chera and Loriguilla formations, the abundance of bivalves decreases from NW to SE i.e., from relatively close to the shore line towards the distal-most part of the carbonate platform. In the Chelva Fm. bivalves are abundant in the Ariño region, interpreted as a palaeogeographic high. The distribution of bivalves might have been largely controlled by the availability of nutrients.
T cell activation is supposed to require two signals via engagement of the TCR and a costimulatory molecule. However, the signaling cascade of costimulatory molecules has remained elusive. Here, I provide evidence that CD44 supports proliferation as well as apoptosis mainly, if not exclusively, by enhancing signal transduction via the TCR/CD3 complex. Blockade of CD44 interferes with mounting of an immune response. This has been demonstrated by the significantly decreased IL-2 production of a T helper line, when stimulated in the presence of a competing CD44 receptor globulin. To evaluate the underlying mechanism, CD44 was cross-linked by an immobilized antibody (IM7). Cross-linking of CD44 induces proliferation of peripheral T cells and apoptosis of thymocytes and a T helper line in the presence of subthreshold levels of anti-CD3. CD44-induced proliferation was accompanied by an upregulation of the activation markers CD25 and CD69 and an increased cytokine production. TCR-mediated apoptosis was accompanied by an upregulation of CD95 ligand and CD95 receptor, which could be greatly enhanced by costimulation via CD44. On the level of signal transduction, coligation of CD44 with CD3 resulted in a strong and sustained increase of early tyrosine phosphorylation events and upregulated downstream signal transduction pathways, such as the ras/ERK and the JNK signaling cascades. These pleiotropic effects of CD44 are due to its involvement in the most proximal events in TCR signaling, as demonstrated by a strong increase in the phosphorylation of the TCR z-chain and ZAP-70. Notably, cross-linking of CD44 was binding-site dependent and was only effective when supporting colocalization of the TCR/CD3 complex and CD44. Cross-linking of CD44 via immobilized IM7 also induced profound changes in cell morphology, characterized by strong adhesion, spreading and development of surface extensions, which were dependent on a functional tubulin and actin cytoskeleton. These cytoskeletal rearrangements were mediated by rac1, a small GTPase of the rho subfamily, and src-family kinases, two of which, fyn and lck, were found to be associated with CD44. By cross-linkage of CD44 these kinases were redistributed into so called lipid rafts. It is supposed that for T cell activation a relocation of the TCR/CD3 complex into the same membrane microdomains is required. The data are interpreted in the sense that the costimulatory function of CD44 relies on its cooperativity with the TCR. Most likely by recruitment of phosphokinases CD44 significantly lowers the threshold for the initiation of signaling via the TCR. The requirement for immobilized anti-CD44, the necessity for neighbouring anti-CD3 and the dependence on the binding site of CD44 strongly suggest that the costimulatory mechanism involves cytoskeletal rearrangements, which facilitate recruitment and redirection of src-family protein kinases in glycolipid enriched membrane microdomains.
At Zwartbas, about 10 km west of Vioolsdrif, southern Namibia, the Dwyka succession is composed of tillites and distal fossiliferous dropstone-bearing glacio-marine shales. The completely exposed Dwyka succession is interbedded with thin bentonites, altered distal pyroclastic deposits, which were derived from the magmatic arc at the southern rim of Gondwana. Dropstone-bearing and dropstonefree sequences intercalate with four diamictites, of which the two lowest were certainly recognised as tillites. Four events of deglaciation were proven at Zwartbas and thus consist with correlative deposits in southern Africa. Numerous fossilised fishes, trace fossils, and plant fragments appear frequently within the lower half of the Dwyka succession whereas trace fossils were principally found in the complete succession. Although the environmental determination is quite problematic, the fossil assemblage rather implies proximal, shallow water conditions with temporary restricted oxygenation. The hinterland was covered with considerable vegetation, which points to a moderate climate. Water salinity determinations based on shale geochemistry rectify contrary palaeontological results and point to rather brackish or non-marine conditions in comparison to present-day salinites. Geochemical analyses of the bentonites relate the pyroclastic deposits with acid to intermediate source magmas, as they are known from the magmatic arc in present-day Patagonia. Tectono-magmatic comparisons furthermore emphasise a syn-collision or volcanic-arc situation of the magma source. However, significant cyclicity in the production of the pyroclastic deposits was not observed. Radiometric age determinations of two tuff beds clearly date the onset of glacial activity into the Late Carboniferous.
More recently, it became clear that conclusions drawn from traditional ecological theory may be altered substantially if the spatial dimension of species interactions is considered explicitly. Regardless of the details of these models, spatially explicit simulations of ecological processes have nearly universally shown that spatial or spatio-temporal patterns in species distributions can emerge even from homogeneous starting conditions; limited dispersal is one of the key factors responsible for the development of such aggregated and patchy distributions (cf., Pacala 1986, Holmes et al. 1994, Molofsky 1994, Tilman 1994, Bascompte and Sole 1995, 1997, 1998, Jeltsch et al. 1999). In line with these ideas, we wish to draw attention to the fact that in heterogeneous landscapes differences in characteristic dispersal distances between species are a sufficient precondition for the emergence of a successional pattern. We will use a simple, spatially explicit simulation program to demonstrate the validity of this statement. We will also show that the speed of the successional progress depends on scale and heterogeneity in the distribution of suitable habitat.
A quantitative model of groundwater flows contributing to the Goblenz state water scheme at the north-western fringe of the Kalahari was developed within this study. The investigated area corresponds to the Upper Omatako basin and encompasses an outer mountainous rim and sediments of the Kalahari sand desert in the centre. This study revealed the eminent importance of the mountainous rim for the water balance of the Kalahari, both in terms of surface and ground water. A hydrochemical subdivision of groundwater types in the mountain rim around the Kalahari was derived from cluster analysis of hydrochemical groundwater data. The western and south-western secondary aquifers within rocks of the Damara Sequence, the Otavi Mountain karst aquifers of the Tsumeb and Abenab subgroups as well as the Waterberg Etjo sandstone aquifer represent the major hydrochemical groups. Ca/Mg and Sr/Ca ratios allowed to trace the groundwater flow from the Otavi Mountains towards the Kalahari near Goblenz. The Otavi Mountains and the Waterberg were identified as the main recharge areas showing almost no or only little isotopic enrichment by evaporation. Soil water balance modelling confirmed that direct groundwater recharge in hard-rock environments tends to be much higher than in areas covered with thick Kalahari sediments. According to the water balance model average recharge rates in hard-rock exposures with only thin sand cover are between 0.1 and 2.5 % of mean annual rainfall. Within the Kalahari itself very limited recharge was predicted (< 1 % of mean annual rainfall). In the Upper Omatako basin the highest recharge probability was found in February in the late rainfall season. The water balance model also indicated that surface runoff is produced sporadically, triggering indirect recharge events. Several sinkholes were discovered in the Otavi Foreland to the north of Goblenz forming short-cuts to the groundwater table and preferential recharge zones. Their relevance for the generation of indirect recharge could be demonstrated by stable isotope variations resulting from observed flood events. Within the Kalahari basin several troughs were identified in the pre-Kalahari surface by GIS-based analyses. A map of saturated thickness of Kalahari sediments revealed that these major troughs are partly saturated with groundwater. The main trough, extending from south-west to north-east, is probably connected to the Goblenz state water scheme and represents a major zone of groundwater confluence, receiving groundwater inflows from several recharge areas in the Upper Omatako basin. As a result of the dominance of mountain front recharge the groundwater of the Kalahari carries an isotopic composition of recharge at higher altitudes. The respective percentages of inflow into the Kalahari from different source areas were determined by a mixing-cell approach. According to the mixing model Goblenz receives most of its inflow (70 to 80 %) from a shallow Kalahari aquifer in the Otavi Foreland which is connected to the Otavi Mountains. Another 15 to 10 % of groundwater inflow to the Kalahari at Goblenz derive from the Etjo sandstone aquifer to the south and from inflow of a mixed component. In conclusion, groundwater abstraction at Goblenz will be affected by measures that heavily influence groundwater inflow from the Otavi Mountains, the Waterberg, and the fractured aquifer north of the Waterberg.
Tropical rain forests and coral reefs are usually regarded as the epitome of complexity and diversity. The mechanisms, however, that allow so many species to coexist continuously, still need to be unraveled. Earlier equilibrium models explain community organization with a strict niche separation and specialization of the single species, achieved mainly by interspecific competition and consecutive resource partitioning. Recent non-equilibrium or stochastic models see stochastic factors ("intermediate disturbances") as more important. Such systems are characterized by broad niche overlaps and an unpredictable species composition. Mechanisms of coexistence are most interesting where species interactions are strongest and species packing is highest. This is the case within a functional group or guild where species use similar resources. In this project a community of seven closely related leaf beetle species (Chrysomelidae: Cassidinae) was investigated which coexist on a common host plant system (fam. Convovulaceae) in a tropical moist savanna (Ivory Coast, Comoé-Nationalpark). A broad overlap in the seasonal phenology of the leaf beetle species stood in contrast to a distinct spatial niche differentiation. The beetle community could be separated in a savanna-group (host plant: Ipomoea) and in a river side group (host plant: Merremia). According to a correspondence analysis the five species at the river side, using a common host plant, Merremia hederacea, proved to be predictable in their species composition. They showed a small scale niche differentiation along the light gradient (microhabitats). Laboratory studies confirmed differences in the tolerance towards high temperatures (up to 50°C in the field). Physiological trade-offs between phenology, microclimate and food quality seem best to describe patterns of resource use of the beetle species. Further a phylogeny based on mt-DNA sequencing of the beetle community was compared to its ecological resource use and the evolution of host plant use was reconstructed
The transmission of proliferative and developmental signals from activated cell-surface receptors to initiation of cellular responses in the nucleus is synergically controlled by the coordinated action of a diverse set of intracellular signalling proteins. The Ras/Raf/MEK/MAPK signalling pathway has been shown to control the expression of genes which are crucial for the physiological regulation of cell proliferation, differentiation and apoptosis. Within this signalling cascade, the Raf protein family of serine/threonine kinases serves as a central intermediate which connects to many of other signal transduction pathways. To elucidate the signalling functions of the different Raf kinases in motoneurons during development, the expression, distribution and subcellular localization of Rafs in the spinal cord and the facial nucleus in brainstem of mice at various embryonic and postnatal stages were investigated. Moreover, we have investigated the intracellular redistribution of Raf molecules in isolated motoneurons from 13 or 14 day old mouse embryos, after addition or withdrawal of neurotrophic factors to induce Raf kinases activation in vitro. Furthermore, in order to investigate the potential anti-apoptotic function of Raf kinases on motoneurons, we isolated motoneurons from B-raf-/- and c-raf-1-/- mouse embryos and analysed the survival and differentiation effects of neurotrophic factors in motoneurons lacking B-Raf and c-Raf-1. We provide evidence here that all three Raf kinases are expressed in mouse spinal motoneurons. Their expression increases during the period of naturally occurring cell death of motoneurons. In sections of embryonic and postnatal spinal cord, motoneurons express exclusively B-Raf and c-Raf-1, but not A-Raf, and subcellularly Raf kinases are obviously colocalized with mitochondria. In isolated motoneurons, most of the B-Raf or c-Raf-1 immunoreactivity is located in the perinuclear space but also in the nucleus, especially after activation by addition of CNTF and BDNF in vitro. We found that c-Raf-1 translocation from the cytosol into the nucleus of motoneurons after its activation by neurotrophic factors is a distinct event. As a central finding of our study, we observed that the viability of isolated motoneurons from B-raf but not c-raf-1 knockout mice is lost even in the presence of CNTF and other neurotrophic factors. This indicates that B-Raf but not c-Raf-1, which is still present in B-raf deficient motoneurons, plays a crucial role in mediating the survival effect of neurotrophic factors during development. In order to prove that B-Raf is an essential player in this scenario, we have re-expressed B-Raf in mutant sensory and motor neurons by transfection. The motoneurons and the sensory neurons from B-raf knockout mouse which were transfected with exogenous B-raf gene revealed the same viability in the presence of neurotrophic factors as primary neurons from wild-type mice. Our results suggest that Raf kinases have important signalling functions in motoneurons in mouse CNS. In vitro, activation causes redistribution of Raf protein kinases, particularly for c-Raf-1, from motoneuronal cytoplasm into the nucleus. This redistribution of c-Raf-1, however, is not necessary for the survival effect of neurotrophic factors, given that B-raf-/- motor and sensory neurons can not survive despite the presence of c-Raf-1. We hypothesize that c-Raf-1 nuclear translocation may play a direct role in transcriptional regulation as a consequence of neurotrophic factor induced phosphorylation and activation of c-Raf-1 in motoneurons. Moreover, the identification of target genes for nuclear translocated c-Raf-1 and of specific cellular functions initiated by this mechanism awaits its characterization.
Biofilm production is an important step in the pathogenesis of S. epidermidis polymer-associated infections and depends on the expression of the icaADBC operon leading to the synthesis of a polysaccharide intercellular adhesin (PIA). The PIA represents a sugar polymer consisting of ß-1,6 linked N-acetyl glucosaminoglycans and mediates the intercellular adherence of the bacteria to each other and the accumulation of a multilayered biofilm. Epidemiological and experimental studies strongly suggest that PIA-production and subsequently biofilm formation contributes significantly to the virulence of specific S. epidermidis strains. This work aimed on the investigation of external factors regulating the ica expression in S. epidermidis. For this purpose, a reporter gene fusion between the ica promoter and the beta-galactosidase gene lacZ from E. coli was constructed and integrated into the chromosome of an ica positive S. epidermidis clinical isolate. The reporter gene fusion was used to investigate the influence of external factors and of sub-MICs of different antibiotics on the ica expression. It was shown that the S. epidermidis biofilm formation is growth phase dependent with a maximum expression in the late logarithmic and early stationary growth phase. The optimal expression was recorded at 42 °C at a neutral pH ranging from 7.0 to 7.5. The glucose content of the medium was found to be essential for biofilm formation, since concentrations of 1.5 to 2 per cent glucose induced the ica expression. In addition, external stress factors as high osmolarity (mediated by 3 to 5 per cent sodium chloride), and sub-lethal concentrations of detergents, ethanol, hydrogene peroxide, and urea significantly enhanced the biofilm production. Subinhibitory concentrations of tetracyline, the semisynthetic streptogramin quinupristin/dalfopristin and the streptogramin growth promoter virginiamycin were found to enhance the ica expression 8 to 11-fold, respectively, whereas penicillin, oxacillin, gentamicin, clindamycin, vancomycin, teicoplanin, ofloxacin, and chloramphenicol had no effects. A weak induction was recorded for sub-MICs of erythromycin. Both quinupristin/ dalfopristin and tetracyline exhibited a strong postexposure effect on the S. epidermidis ica expression, respectively, even when the substances were immediately removed from the growth medium. The results were confirmed by Northern blot analysis of the ica transcription and quantitative analysis of biofilm formation in a colorimetric assay. Expression of the icaprom::lacZ reporter gene plasmid in Bacillus subtilis and S. epidermidis revealed that the ica induction by sub-MICs of streptogramins and tetracycline might depend on unidentified regulatory elements which are specific for the staphylococcal cell. In contrast, the activation by external stress signals seems to be mediated by factors which are present both in Staphylococci and in Bacillus subtilis. Construction and analysis of an agr-mutant in a biofilm-forming S. epidermidis strain excluded the possibility that the Agr-quorum-sensing system significantly contributes to the ica expression in the stationary growth phase. However, clear evidence was provided that in S. aureus the ica transcription depends on the expression of the alternative transcription factor sigmaB, which represents a global regulator of the stress response in S. aureus as well as in B. subtilis. For this purpose, a sigB knockout mutant had been constructed in a biofilm-forming S. aureus. This mutant showed a markedly decrease of the ica transcription and biofilm-production, whereas a complement strain carrying the sigB gene on an expression vector completely restored the biofilm-forming phenotype of the S. aureus wild type. Southern blot analysis indicated that the the sigB gene is also present in S. epidermidis and Northern analyses of the sigB and the ica transcription revealed that both genes are activated under identical conditions (i. e. in the stationary growth phase and by external stress factors) suggesting a similar regulatory pathway as in S. aureus. However, since neither in S. aureus nor in S. epidermidis the ica promoter has obvious similiarities to known SigB-dependent promotoer sequences it is tempting to speculate that the ica activation is not directely mediated by SigB, but might be indirectely controlled by other SigB-dependent regulatory elements which remain to be elucidated.