Seep communities from two mud volcanoes in the deep eastern Mediterranean Sea: faunal composition, spatial patterns and environmental control

The Mediterranean Sea constitutes a unique environment to study cold-seep ecosystems due to the presence of different geodynamic settings, from an active margin along the Mediterranean Ridge (MR) to a passive margin in the Nile Deep-Sea Fan (NDSF). We attempted to identify the structure of benthic communities associated with the Napoli and Amsterdam mud volcanoes (MVs) located on the MR and to establish the links between faunal distribution and environmental conditions at different spatial scales. Comparison between the 2 MVs revealed that the faunal distribution seemed to be mainly controlled by the characteristics of the microhabitats. On both geological structures, the variability between the different microhabitats was higher than the variability observed between replicates of the same microhabitat, and the distribution of macro-fauna was apparently linked to gradients in physico-chemical conditions. The peripheral sites from Napoli were generally more oxygenated and harboured lower species richness than the active sites. The reduced sediment microhabitat from Amsterdam presented the highest methane concentrations and was mainly colonised by symbiont-bearing vesicomyid bivalves and heterotrophic dorvilleid polychaetes. Overall, a higher taxonomic diversity was observed on Napoli. Sub-stratum type was hypothesised to be the second factor influencing faunal distribution. The results of this study highlight the high heterogeneity of faunal communities associated with seep ecosystems within this region and the need to pursue investigations at various spatial and temporal scales.

Etude sanitaire de la zone 17.48 de Fouras. Charente-Maritime

Suite à la demande d’exploitation de la zone de Fouras, n°17.48 par le Comité Régional de la Conchyliculture du Poitou-Charentes (CRCPC), la Direction Départementale des Territoires et de la Mer (DDTM) a demandé la réalisation d’une étude sanitaire en vue du classement de la zone de production de coquillages pour les bivalves fouisseurs (groupe 2). Cette étude réalisée par le Laboratoire Environnement Ressources des Pertuis Charentais (LER/PC) bénéficie d’un financement de la Direction Générale de l 'Alimentation (DGAL). Basée sur les paramètres microbiologiques (Escherichia coli) et chimiques (plomb, mercure, cadmium), l’étude sanitaire a pour objectifs d'estimer la qualité microbiologique et chimique de la zone en vue du classement sanitaire de la zone par l'administration conformément aux exigences du Règlement CE n° 854/2004 ; et de déterminer la stratégie d'échantillonnage à mettre en oeuvre dans le cadre de la surveillance sanitaire régulière de cette zone suite à son classement. L’étude des informations disponibles a permis l’identification de sources de contamination potentielle et la définition d’une stratégie d’échantillonnage. Deux points de suivis ont été positionnés dans les secteurs jugés sensibles aux sources de contamination et ont été échantillonnés du 29 juillet 2011 au 4 octobre 2012. Les concentrations maximales en cadmium, mercure et plomb sont inférieures aux critères chimiques réglementaires et sont compatibles avec un classement A, B ou C. Le suivi microbiologique réalisé indique une qualité B pour chacun des deux points de suivi. La qualité de la zone semble donc homogène, et est estimée B dans son ensemble. Le point « Les Ecussons » est le plus sensible aux contaminations microbiologiques, la surveillance régulière REMI de la zone du Fier d’Ars pour le groupe 2 sera donc basée sur ce point.

Oberjurassische Korallen-Geschiebe (Thamnasteria concinna) aus einer Kies-/Sandgrube bei Freden/Leine (Leinebergland)

Upper-Jurassic geschiebe-corals (Thamnasteria concinna) from a gravel-/sandpit at Freden/Leine are described. They are slightly bored by bivalves (Gastrochaenolites) and worms (Trypanites). Some oysters (Nanogyra Inana) encrusted the surface. The corals growed as massiv head-like (bulbous) colonies with "multicolumnar growth form" and ragged outlines. Similar shaped colonies are reported from Easteuropean Upper Jurassic (Pommerania), but are never reported for NW-Germany. Beds in which the coral-geschiebe were found - Drenthe stage in age - contain a high content of local geschiebe-material. The low degree of abrasion of the coral-geschiebe indicates short glacial transportation. It is possible, that the geschiebe originate from the Heersumer Schichten from Selter to Thüster Berg.

Etude sanitaire de la zone 17.52 - Ronce les Bains - Barat, Charente-Maritime

Suite à la demande d'exploitation de la zone de Ronce les Bains – Barat par le Comité Régional de la Conchyliculture du Poitou-Charentes (CRCPC), la Direction Départementale du Territoire et de la Mer (DDTM) a demandé la réalisation d'une étude sanitaire en vue du classement de cette zone de production pour les bivalves fouisseurs (groupe 2). Cette étude réalisée par le Laboratoire Environnement Ressources des Pertuis Charentais bénéficie d'un financement de la Direction Générale de l'Alimentation (DGAL). Basée sur le paramètre microbiologique (Escherichia coli) et chimiques (plomb, mercure, cadmium). L'étude sanitaire a pour objectifs : d'estimer la qualité microbiologique et chimique de la zone en vue du classement sanitaire de la zone par l'administration conformément aux exigences du Règlement CE n° 854/2004 ; et de déterminer la stratégie d'échantillonnage à mettre en oeuvre dans le cadre de la surveillance sanitaire régulière de cette zone suite à son classement. L’étude des informations disponibles a permis l’identification de sources de contamination potentielle et la définition d’une stratégie d’échantillonnage. Trois points de suivi ont été positionnés dans des secteurs jugés sensibles aux sources de contamination, et ont été échantillonnés de février 2011 à janvier 2013. Les concentrations maximales en cadmium, mercure et plomb sont inférieures aux critères chimiques réglementaires et sont compatibles avec un classement A, B ou C. Le suivi microbiologique réalisé indique une qualité B pour chacun des deux points de suivi selon les seuils microbiologiques définis par le règlement (CE) n° 854/2004 (un troisième point a été arrêté au cours de l’étude pour manque de ressource). La qualité de la zone est donc estimée B dans son ensemble. Le point « Ronce » est le plus sensible aux contaminations microbiologiques, la surveillance régulière REMI de la zone de Ronce les Bains – Barat pour le groupe 2 sera donc basée sur ce point.

Etude sanitaire de la zone 17.51 de Bourgeois. Charente-Maritime.

Suite à la demande d’exploitation de la zone de Bourgeois par les professionnels, la Direction Départementale du Territoire et de la Mer (DDTM) a demandé la réalisation d’une étude sanitaire en vue du classement de cette zone de production pour les bivalves fouisseurs (groupe 2 ).Cette étude réalisée par le Laboratoire Environnement ressources des Pertuis Charentais bénéficie d’un financement de la Direction Générale de l’Alimentation (DGAL). Basée sur le paramètre microbiologique (Escherichia coli) et chimiques (plomb, mercure, cadmium), l’étude sanitaire a pour objectifs : d’estimer la qualité microbiologique et chimique de la zone en vue du classement sanitaire de la zone par l’administration conformément aux exigences du Règlement CE n° 854/2004 ; et de déterminer la stratégie d’échantillonnage à mettre en œuvre dans le cadre de la surveillance sanitaire régulière de cette zone suite à son classement. L’étude des informations disponibles a permis l’identification de sources de contamination potentielle et la définition d’une stratégie d’échantillonnage. Trois points de suivi ont été positionnés dans des secteurs jugés sensibles aux sources de contamination et ont été échantillonnés du 21 juillet 2011 au 20 août 2012. Les concentrations maximales en cadmium, mercure et plomb sont inférieures aux critères chimiques réglementaires et sont compatibles avec un classement en A, B ou C. Le suivi microbiologique réalisé indique une qualité B pour chacun des trois points de suivi selon les seuils microbiologiques définis par le règlement (CE) n° 854/2004. La qualité de la zone est donc estimée B dans son ensemble. Le point « Bonnemort » est retenu pour la surveillance régulière REMI du groupe 2 dans la zone n° 17-51 Bourgeois.

Verteilungsmuster der Mesofauna im hohen Ober-Hauterive Nordwestdeutschlands

The vertical distribution pattem of mesofaunal elements is described from clay-marl bedding rhythms from the Frielingen section (Hannover, NW Germany), which exposes latest Hau- terivian sediments (early Cretaceous). Some mesofaunal groups show a correlation with the pale- dark bedding rhythms. The pale, marly beds are chracterised by bryozoans. In addition remnants of crinoids, echinoids, asteroids, ophiuroids and holothuroids are more common in pale layers than in dark ones. Converseley, the relative abundance of serpulids, fish remains, bivalves and gastropods shows no relationship to the bedding rhythms.

Identificação do potencial renovável para produção de electricidade na perspectiva da microgeração

Tese submetida à Universidade de Lisboa, Faculdade de Ciências e aprovada em provas públicas para a obtenção do Grau de Doutor em Energia e Ambiente (especialidade em Energia e Desenvolvimento Sustentável).

Induction of apoptosis by UV in the flat oyster, Ostrea edulis

Apoptosis is a fundamental feature in the development of many organisms and tissue systems. It is also a mechanism of host defense against environmental stress factors or pathogens by contributing to the elimination of infected cells. Hemocytes play a key role in defense mechanisms in invertebrates and previous studies have shown that physical or chemical stress can increase apoptosis in hemocytes in mollusks. However this phenomenon has rarely been investigated in bivalves especially in the flat oyster Ostrea edulis. The apoptotic response of hemocytes from flat oysters, O. edulis, was investigated after exposure to UV and dexamethasone, two agents known to induce apoptosis in vertebrates. Flow cytometry and microscopy were combined to demonstrate that apoptosis occurs in flat oyster hemocytes. Investigated parameters like intracytoplasmic calcium activity, mitochondrial membrane potential and phosphatidyl-serine externalization were significantly modulated in cells exposed to UV whereas dexamethasone only induced an increase of DNA fragmentation. Morphological changes were also observed on UV-treated cells using fluorescence microscopy and transmission electron microscopy. Our results confirm the apoptotic effect of UV on hemocytes of O. edulis and suggest that apoptosis is an important mechanism developed by the flat oyster against stress factors.

Produção biológica integrada de hidrogénio e metano a partir de resíduos da indústria do biodiesel

Dissertação de Mestrado Integrado em Engenharia da Energia e do Ambiente

Relatório da Comissão Geológica do Reino acerca da viagem feita aos diversos países da Europa pelo Membro Carlos Ribeiro em 1858

Relatório original, datado de 31 de Janeiro de 1859, do espólio do "Arquivo Histórico do LNEG"

Isotope and fatty acid trends along continental shelf depth gradients: Inshore versus offshore hydrological influences on benthic trophic functioning

Anthropogenic activities and land-based inputs into the sea may influence the trophic structure and functioning of coastal and continental shelf ecosystems, despite the numerous opportunities and services the latter offer to humans and wildlife. In addition, hydrological structures and physical dynamics potentially influence the sources of organic matter (e.g., terrestrial versus marine, or fresh material versus detrital material) entering marine food webs. Understanding the significance of the processes that influence marine food webs and ecosystems (e.g., terrestrial inputs, physical dynamics) is crucially important because trophic dynamics are a vital part of ecosystem integrity. This can be achieved by identifying organic matter sources that enter food webs along inshore–offshore transects. We hypothesised that regional hydrological structures over wide continental shelves directly control the benthic trophic functioning across the shelf. We investigated this issue along two transects in the northern ecosystem of the Bay of Biscay (north-eastern Atlantic). Carbon and nitrogen stable isotope analysis (SIA) and fatty acid analysis (FAA) were conducted on different complementary ecosystem compartments that include suspended particulate organic matter (POM), sedimentary organic matter (SOM), and benthic consumers such as bivalves, large crustaceans and demersal fish. Samples were collected from inshore shallow waters (at ∼1 m in depth) to more than 200 m in depth on the offshore shelf break. Results indicated strong discrepancies in stable isotope (SI) and fatty acid (FA) compositions in the sampled compartments between inshore and offshore areas, although nitrogen SI (δ15N) and FA trends were similar along both transects. Offshore the influence of a permanently stratified area (described previously as a “cold pool”) was evident in both transects. The influence of this hydrological structure on benthic trophic functioning (i.e., on the food sources available for consumers) was especially apparent across the northern transect, due to unusual carbon isotope compositions (δ13C) in the compartments. At stations under the cold pool, SI and FA organism compositions indicated benthic trophic functioning based on a microbial food web, including a significant contribution of heterotrophic planktonic organisms and/or of SOM, notably in stations under the cold pool. On the contrary, inshore and shelf break areas were characterised by a microalgae-based food web (at least in part for the shelf break area, due to slope current and upwelling that can favour fresh primary production sinking on site). SIA and FAA were relevant and complementary tools, and consumers better medium- to long-term system integrators than POM samples, for depicting the trophic functioning and dynamics along inshore–offshore transects over continental shelves.

Estudo de viabilidade para a instalação de uma central piloto para geração de energia elétrica a partir de biomassa na ilha do Príncipe (R.D. de S. Tomé e Príncipe)

O referido projeto tem como objetivo principal a avaliação das capacidades técnicas, económicas e ambientais da ilha do Príncipe (República democrática de S. Tomé e Príncipe) para possibilitar a instalação de uma central piloto (500 kW) de produção de energia elétrica a partir de biomassa captada proveniente de la floresta (resíduos florestais) e campos agrícolas(resíduos agrícolas) com intuito de aumentar a potência total instalada na ilha. S. Tomé e Príncipe é um país subdesenvolvido e partilha de um dos maiores problemas dos países dessa categoria, a precária produção e distribuição da energia elétrica a população. Em S. Tomé e Príncipe estes problemas são derivados a fraca potência instalada e dependência de combustíveis fósseis. Especificamente na ilha do Príncipe, a situação é ainda mais complicada, situação prendesse com o facto de que o transporte de combustível da Ilha de S. Tomé para a ilha do Príncipe não se processar num regime contínuo, devido ao aumento do consumo pela população da Ilha do Príncipe conjugado com a fraca potência instalada e a falta de condições ideais de armazenamento de combustível, o que origina muitas falhas na distribuição de eletricidade ou uma racionalidade na sua distribuição. A racionalidade de distribuição de eletricidade na ilha do Príncipe segue o princípio de fornecimento em momentos de maior necessidade, isto é: horários em que as famílias se encontram juntas em suas casas (18 as 24h), períodos de maior produtividade da ilha (8 as 12h), com interregnos de várias horas na distribuição. Este princípio não respeita instituições como os hospitais onde a necessidade de energia elétrica permanente é uma necessidade. Outra motivação para a elaboração deste projeto é o facto de que a ilha do Príncipe a partir de ano 2012 passou a ser uma reserva da Biosfera da UNESCO. Este facto obrigou obviamente a ilha do Príncipe a ter uma maior preocupação com a sustentabilidade ambiental. Perante essas necessidades, surgiu a necessidade de criação de um projeto que tentasse cobrir as lacunas elétricas da Ilha do Príncipe. O projeto é ambicioso, não só para S. Tomé e Príncipe, mas também para todos os países da região e principalmente aqueles com grande potencialidade em biomassa florestal e agrícola.

Climate Change Influences Carrying Capacity in a Coastal Embayment Dedicated to Shellfish Aquaculture

A spatially explicit coupled hydrodynamic-biogeochemical model was developed to study a coastal ecosystem under the combined effects of mussel aquaculture, nutrient loading and climate change. The model was applied to St Peter's Bay (SPB), Prince Edward Island, Eastern Canada. Approximately 40 % of the SPB area is dedicated to mussel (Mytilus edulis) longline culture. Results indicate that the two main food sources for mussels, phytoplankton and organic detritus, are most depleted in the central part of the embayment. Results also suggest that the system is near its ultimate capacity, a state where the energy cycle is restricted to nitrogen-phytoplankton-detritus-mussels with few resources left to be transferred to higher trophic levels. Annually, mussel meat harvesting extracts nitrogen (N) resources equivalent to 42 % of river inputs or 46.5 % of the net phytoplankton primary production. Under such extractive pressure, the phytoplankton biomass is being curtailed to 1980's levels when aquaculture was not yet developed and N loading was half the present level. Current mussel stocks also decrease bay-scale sedimentation rates by 14 %. Finally, a climate change scenario (year 2050) predicted a 30 % increase in mussel production, largely driven by more efficient utilization of the phytoplankton spring bloom. However, the predicted elevated summer temperatures (> 25 A degrees C) may also have deleterious physiological effects on mussels and possibly increase summer mortality levels. In conclusion, cultivated bivalves may play an important role in remediating the negative impacts of land-derived nutrient loading. Climate change may lead to increases in production and ecological carrying capacity as long as the cultivated species can tolerate warmer summer conditions.

Quantificação de iodo em alimentos consumidos em Portugal: resultados preliminares

O iodo é um oligoelemento indispensável para a síntese das hormonas da tiroide. A alimentação é a maior fonte natural de iodo. Assim, o principal objetivo deste trabalho foi a determinação de iodo em alimentos como consumidos e representativos da dieta portuguesa. A metodologia escolhida para a quantificação deste nutriente foi a espectrometria de massa acoplada ao plasma indutivo (ICP-MS). Analisaram-se seis grupos de alimentos: peixes, mariscos e bivalves, leite e derivados, vegetais, fruta e refeições compostas. Os grupos do pescado (peixe, marisco e bivalves) foram os que apresentaram concentrações de iodo mais elevados, com um valor médio de 114 μg/100g. Os laticínios são também uma fonte importante para suprir o aporte diário de iodo (150 μg/dia) apresentado valores médios de 22 μg/100g. Os resultados permitem concluir que em Portugal uma alimentação rica em pescado e lacticínios supre a dose diária recomendada de iodo para um adulto saudável.

Riffe und fazielle Entwicklung der florigemma-Bank (Korallenoolith, Oxfordium) im Süntel und östlichen Wesergebirge (NW-Deutschland

During the Sedimentation of the platform carbonate deposits of the Korallenoolith Formation (middle Oxfordian to early Kimmeridgian) small buildups ofcorals formed in the Lower Saxony Basin. These bioconstructions are restricted to particular horizons (Untere Korallenbank,ßorigenuna-Bank Member etc.) and represent patch reefs and biostromes. In this study, the development of facies, fossil assemblages, spatial distribution of fossils, and reefs of the ßorigenuna-Bank Member (upper Middle Oxfordian) in the Süntel Mts and the eastern Wesergebirge Mts is described; the formation of reefs is discussed in detail. Twelve facies types are described and interpreted. They vary between high-energy deposits as well winnowed oolites and quiet-water lagoonal mudstones. Owing to the significance of biota, micro- and macrofossils are systematically described. The reefs are preserved in growth position, are characterized by numerous corresponding features and belong to a certain reef type. According to their size, shape and framework, they represent patch reefs, coral knobs (sensu James, 1983), coral thrombolite reefs (sensu Leinfelder et al., 1994) or “Klein- and Mitteldickichte” (sensu Laternser, 2001). Their growth fabric corresponds to the superstratal (dense) pillarstone (sensu Insalaco, 1998). As the top of the ßorigenuna-Bank displays an erosional unconformity (so-called Hauptdiskontinuität), the top of the reefs are erosionally capped. Their maximum height amounts to at least the maximum thickness of the ßorigenuna-Bank which does not exceed 4 metres. The diversity of coral fauna of the reefs is relatively low; a total of 13 species is recorded. The coral community is over- whelmingly dominated by the thin-branched ramose Thamnasteria dendroidea (Lamouroux) that forms aggregations of colonies (77?. dendroidea thickets). Leafy to platy Fungiastrea arachnoides (Parkinson) and Thamnasteria concinna (Goldfuss) occur subordinately, other species are only of minor importance. In a few cases, the reef-core consisting of Th. dendroidea thickets is laterally encrusted by platy F. arachnoides and Th. concinna colonies, and microbial carbonates. This zonation reflects probably a succession of different reef builders as a result of changing environmental conditions (allogenic succession). Moreover, some reefs are overlain by a biostrome made of large Solenopora jurassica nodules passing laterally in a nerinean bed. Mikrobial carbonates promoted reef growth and favoured the preservation of reef organismn in their growth position or in situ. They exhibit a platy, dendroid, or reticulate growth form or occur as downward-facing hemispheroids. According to their microstructure, they consist of a peloidal, clotted, or unstructured fabric (predominately layered and poorly structured thrombolite as well as clotted leiolite) (sensu Schmid, 1996). Abundant endo- and epibiontic organisms (bivalves, gastropods, echinoids, asteroids, ophiuroids, crabs etc) are linked to the reefs. With regard to their guild structure, the reefs represent occurrences at which only a few coral species serve as builder. Moreover, microbial carbonates contribute to both building and binding of the reefs. Additional binder as well as baffler are present, but not abundant. According to the species diversity, the dweller guild comprises by far the highest number of invertebrate taxa. The destroyer guild chiefly encompasses bivalves. The composition of the reef community was influenced by the habitat structure of the Th. dendroidea thickets. Owing to the increase in encrusting organisms and other inhabitants of the thickets, the locational factors changed, since light intensity and hydrodynamic energy level and combined parameters as oxygen supply declined in the crowded habitat. Therefore a characteristic succession of organisms is developed that depends on and responds to changing environmental conditions („community replacement sequence“). The succession allows the differentiation of different stages. It started after the cessation of the polyps with boring organisms and photoautotrophic micro-encrusters (calcareous algae, Lithocodium aggregatum). Following the death of these pioneer organisms, encrusting and adherent organisms (serpulids, „Terebella“ species, bryozoans, foraminifers, thecideidinids, sklerospongid and pharetronid sponges, terebratulids), small mobile organisms (limpets), and microbial induced carbonates developed. The final stage in the community replacement sequence gave rise to small cryptic habitats and organisms that belong to these caves (cryptobionts, coelobites). The habitat conditions especially favoured small non-rigid demosponges (“soft sponges”) that tolerate reduced water circulation. Reef rubble is negligible, so that the reefs are bordered by fossiliferous micritic limestone passing laterally in micritic limestone. Approximately 10% of the study area (outcropping florigemma-Bank) corresponds to reefal deposits whereas the remaining 90% encompass lagoonal inter-reefal deposits. The reef development is a good example for the interaction between reef growth, facies development and sea-level changes. It was initiated by a sea-level rise (transgression) and corresponding decrease in the hydrodynamic energy level. Colonization and reef growth took place on a coarse-grained Substrate composed of oncoids, larger foraminifers and bioclasts. Reef growth took place in a calm marine lagoonal setting. Increasing abundance of spherical coral morphs towards the Northeast (section Kessiehausen, northwestem Süntel Mts) reflects higher turbidity and a facies transition to coral occurrences of the ßorigenuna-Bank Member in the adjacent Deister Mts. The reef growth was neither influenced by stonns nor by input of siliciclastic deposits, and took place in short time - probably in only a thousand years under most probably mesotrophic conditions. The mass appearance of solenoporids and nerineids in the upper part of the ßorigenuna-Bank Member point to enhanced nutrient level as a result of regression. In addition, this scenario of fluctuations in nutrient availability seems to be responsible for the cessation of reef corals. The sea level fall reached its climax in the subaerial exposure and palaeokarst development of the florigemma-Bank. The reef building corals are typical pioneer species. The blade-like, flattened F. amchnoides colonies are characterized by their light porous calcium carbonate skeleton, which is a distinct advantage in soft bottom environment. Thus, they settled on soft bottom exposing the large parts of its surface to the incoming light. On the other hand, in response to their light requirements they were also able to settle shaded canopy structures or reef caves. Th. dendroidea is an opportunistic coral species in very shallow, well illuminated marine environment. Their thin and densely spaced branches led to a very high surface/volume ratio of the colonies that were capable to exploit incoming light due to their small thamasterioid calices characterized by “highly integrated polyps”. In addition, sideward coalescence of branches during colony growth led to a wave-resistant framework and favoured the authochthonous preservation of the reefs. Asexual reproduction by fragmented colonies promoted reef development as Th. dendroidea thickets laterally extend over the sea floor or new reefs have developed from broken fragments of parent colonies. Similar build ups with Th. dendroidea as a dominant or frequent reef building coral species are known from the Paris Basin and elsewhere from the Lower Saxony Basin (Kleiner Deister Mts). These buildups developed in well-illuminated shallow water and encompass coral reefs or coral thrombolite reefs. Intra- and inter-reef deposits vary between well-winnowed reef debris limestone and mudstones representing considerably calmer conditions. Solenoporid, nerineids and diceratides belong to the characteristic fossils of these occurrences. However, diceratides are missing in theflorigemma-Bank Member. Th. dendroidea differs in its colonization of low- to high-energy environment from recent ramose scleractinian corals (e.g., Acropora and Porites sp.). The latter are restricted to agitated water habitats creating coral thickets and carpets. According to the morphologic plasticity of Th. dendroidea, thick-branched colonies developed in a milieu of high water energy, whereas fragile, wide- and thin-branched colonies prevail in low-energy settings. Due to its relatively rapid growth, Th. dendroidea was able to keep pace with increased Sedimentation rates. 68 benthonic foraminiferan species/taxa have been recognized in thin sections. Agglutinated foraminifers (textulariids) predominate when compared with rotaliids and milioliids. Numerous species are restricted to a certain facies type or occur in higher population densities, in particular Everticyclammina sp., a larger agglutinated foraminifer that occurs in rock building amounts. Among the 25 reef dwelling foraminiferal species, a few were so far only known from Late Jurassic sponge reefs. Another striking feature is the frequency of adherent foraminiferal species. Fauna and flora, in particular dasycladaleans and agglutinated foraminifers, document palaeobiogeographic relationships to the Tethys and point to (sub)tropical conditions. Moreover, in Germany this foraminiferan assemblage is yet uncompared. In Southern Germany similar tethyan type assemblages are not present in strata as young as Middle Tithonian.