凹顶藻次级代谢产物及其生物活性和化学分类学研究

本论文对近10年凹顶藻中分离鉴定的146个结构新颖的次级代谢产物及其生物活性和结构鉴定技术进行了总结，并对采自中国沿海的马岛凹顶藻、俯仰凹顶藻、冈村凹顶藻、复生凹顶藻、齐腾凹顶藻、羽枝凹顶藻、三列凹顶藻和似瘤凹顶藻的次级代谢产物进行了提取分离，结构鉴定，生物活性筛选和化学分类学探讨。 干燥并粉碎的8种凹顶藻样品分别进行有机溶剂提取，粗提物进行硅胶柱、凝胶sephadex LH-20柱、制备薄层和高效液相等色谱方法分离纯化得单体化合物，利用核磁共振和质谱等现代谱学技术鉴定化合物的结构，共计分离鉴定139个化合物，其中新化合物33个，新天然产物6个，部分化合物由不同种中多次分离鉴定，结构类型涵盖倍半萜、二萜、三萜、C15-聚乙酰、吲哚和甾体类等，并且大多为卤代结构。 生物活性筛选和文献检索结果表明，8种凹顶藻的部分次级代谢产物，特别是大量存在的卤代化合物，具有抗菌、细胞毒和拒食杀虫等多种生物活性。 化学分类学分析表明，8种凹顶藻的次级代谢产物，特别是丰富的卤代结构，可为其分类学研究提供重要的分子证据。

三种海洋红藻和两株放线菌次级代谢产物研究

海洋是一个巨大的天然产物宝库，约占地球表面积70%的海洋蕴藏着80%的生物资源。由于海洋生态环境的特殊性，导致海洋生物能够产生大量结构独特多变和活性特殊多样的代谢产物。我国海域辽阔，海洋资源丰富，为寻找结构新颖、生理活性独特的先导化合物，加强对海洋资源的开发利用，本论文对中国沿海的三种海洋红藻和两株放线菌次生代谢产物以及生物活性进行研究，为新药研究与开发提供模式结构和药物前体。 对红藻似瘤凹顶藻Laurencia similis乙酸乙酯萃取物进行分离纯化，从中得到单体化合物35个，通过波谱学方法（IR、MS、NMR等）鉴定了他们的结构。分别为：2, 2, 5, 5, 6, 6-sixibromo-3, 3-bi-1H-indole (1)，3,5-dibromo- 1-methyl-indole (2)，3',5',6,6'-tetrabromo-2,4-dimmethyldiphenyl ether (3)，1,2,5- tribromo-3-bromoamino-7-bromomethylnaphthalene (4)，2,5,8-tribromo-3-bromo- amino-7-bromomethylnaphthalene (5)，2,5,6-tribromo-3-bromoamino-7-bromo- methylnaphthalene (6), 2,5,6,5',6'-pentabromo-3,4,3',4'-tetramethoxybenzophenone (7), (4E)-1-bromo-5-[(1'S*,3'R*)-3'-bromo-2',2'-dimethyl-6'-methylenecyclohexyl] -3-methylpent-4-ene-2,3-diol (8)，4-hydroxy-Palisadin C (9)，Isopalisol (10)，Luzonensol (11)，Palisadin B (12)，Aplysistatin (13)，Palisadin A (14)，5-Acetoxypalisadin B (15)，Aristolan-1(10)- en-9-ol (16)，Aristol-8-en-1-one (17)，Aristolan-9-en-1-one (18)，Aristolan-1(10)-en- 9-one (19)，Aristofone (20)，Aristolan-1(10)-8-diene (21)，Aristolan-1,9-diene (22)，10-Hydroxyaristolan-9-one (23)，7,11,15-trimethyl-3-methylene-hexadecan-1,2-diol (24)，3β-Hydroxyergosta- 5,24(28)-dien-7-one (25)，Isofucosterol (26)，β-sitosterol (27)，豆甾-4-烯-3α,6β-二醇 (28)，Cholesta-5-en-3β-ol (29)，Stigmasterol (30)，2,3,5,6-四溴-吲哚 (31)，2,3,6-tribromo-1H-indole (32)，3,5,6-tribromo-1-methylindole (33)，3,5,6-tribromo -1H-indole (34)，2,3,5-tribromo-1-methylindole (35)，其中化合物1-9为新化合物，化合物10-15、20和化合物24-30均为首次从该种海藻中得到。对新化合物1-9进行PTP1B酶抑制剂活性筛选，新化合物1、3、7显示强的PTP1B酶抑制活性。 对红藻齐藤凹顶藻Laurencia saitoi乙酸乙酯萃取物进行分离纯化，从中得到单体化合物11个，通过波谱学方法（IR、MS、NMR等）鉴定了他们的结构，分别为：2-hydroxyl-Luzofuranone (1)，2-hydroxyl-Luzofuranone B (2)，4-hydroxyl-Palisudin C (3)，2-bromo-γ-ionone (4)，Aplysistatin (5)，5-Acetoxypalisadin B (6)，Palisadin B (7)，Palisadin A (8)，Pacifigorgiol (9)，豆甾-4-烯-3α,6β-二醇 (10)，2, 3, 5, 6-四溴-吲哚 (11)，其中化合物1-4为新化合物，所有化合物均为首次从该种海藻中得到。通过MTT法对分离得到的新化合物1-4进行肿瘤细胞毒活性筛选，结果显示4个新化合物对所测肿瘤细胞株均无明显的活性。 对红藻瘤状软骨凹顶藻Chondrophycus papillous乙酸乙酯萃取物进行分离纯化，从中得到单体化合物5个，通过波谱学方法（MS、NMR等）鉴定了他们的结构，分别为邻苯二甲酸二丁酯 (1)，邻苯二甲酸二异辛酯 (2)，胆甾醇 (3)，3,7,11,15-tetramethyl-hexadec-2-en-1-ol (4)，4-羟基苯甲醛 (5)，所有化合物均为首次从该种海藻中得到。 对海洋放线菌M159乙酸乙酯萃取物进行分离纯化，从中得到单体化合物13个，通过波谱学方法（MS、NMR等）鉴定了他们的结构，分别为：5-(4',6'-dihydroxy-6-methyloctyl)furan-2(5H)-one (A)，phenethyl alcohol (1)，4-羟基苯甲醛(2)，anthranilic acid (3)，4-Hydroxy-3-methoxy- phenyl-propionic acid (4)，5-(6,7-dihydroxy-6-methyloctyl)furan-2(5H)-one (5)，p-Hydroxyphenylethyl alcohol (6)，3-Indoleacrylic acid (7)，Indol-3-carboxylic acid (8)，Adenine cordyceposide (9)，腺嘌呤核苷(10)，尿嘧啶核苷(11)，Thymidine (12)，其中化合物A为新化合物。所有化合物均为首次从该株放线菌中得到。 对海洋放线菌L211乙酸乙酯萃取物进行分离纯化，从中得到单体化合物15个，通过波谱学方法（MS、NMR等）鉴定了7个结构，分别为：spatozoate (1)，anthranilic acid (2)，3-Indolylethanol (3)，1-Acetyl-β-carbolin (4)，p-Hydroxyphen- ylethyl alcohol (5)，Indole-3-acetic acid (6)，Indol-3-carboxylic acid (7)，所有化合物均为首次从该株放线菌中得到。

Taxonomy and phylogeny of Osmundea (Rhodomelaceae, Rhodophyta) in Atlantic Europe

Two species of Osmundea Stackhouse (Rhodomelaceae, Rhodophyta) that occur in Atlantic Europe have been confused under the names Osmundea ramosissima (Oeder) Athanasiadis and Osmundea truncata (Kutzing) Nam et Maggs, regarded until now as a synonym of O. ramosissima, An epitype from its type locality (Stavanger, Norway) is selected for Osmundea ramosissima Athanasiadis, recognized here as a valid name for Fucus ramosissimus Oeder, nom. illeg. Details of vegetative and reproductive morphology of O. ramosissima are reported, based on material from France, the British Isles, and Helgoland. Osmundea ramosissima resembles other species of Osmundea in its vegetative axial segments with two pericentral cells and one trichoblast, spermatangial development from apical and epidermal cells (filament type), the formation of five pericentral cells in the procarp-bearing segment of the female trichoblast, and tetrasporangial production from random epidermal cells. Among the species of Osmundea, O. ramosissima is most similar to O. truncata. Both species have discoid holdfasts, secondary pit connections between epidermal cells, and cup-shaped spermatangial pits. They differ in that: (a) O. ramosissima lacks lenticular wail thickenings and refractive needle-like inclusions in medullary cells, both of which are present in O. truncata; (b) O. ramosissima has branched spermatangial filaments that terminate in a cluster of several cells, whereas in O. truncata the unbranched spermatangial filaments have a single large terminal sterile cell; and (c) cystocarps of O. ramosissima lack protuberant ostioles but ostioles are remarkably protuberant in o. truncata. Phylogenetic analyses of rbcL sequences of Laurencia obtusa (Hudson) Lamouroux and all five Atlantic European species of Osmundea, including the type species, strongly support the generic status of Osmundea. Osmundea ramosissima and O. truncata are closely related (5.2% sequence divergence) and form a well-supported clade sister to a clade consisting of O. pinnatifida (Hudson) Stack-house, O. osmunda Stackhouse and O. hybrida (A. P. de Candolle) Nam. The formation of secondary pit connections between epidermal cells is a synapomorphy for the O. ramosissima + O. truncata clade. The close relationship between species with cup-shaped spermatangial pits (Osmundea hybrida) and urn-shaped pits (Osmundea pinnatifida and Osmundea osmunda) shows that spermatangial pit shape is not an important phylogenetic character. Parsimony analysis of a morphological data set also supports the genus Osmundea but conflicts with the molecular trees in infrageneric relationships, placing O. hybrida basal within the Osmundea clade and grouping O. osmunda and O. pinnatifida but not O. truncata and O. ramosissima. A key to Osmundea species is presented.

RS dos estudantes do curso de licenciatura em enfermagem sobre cuidados hospitalares e cuidados comunitários

Tema e Referencial teórico: Nas escolas, se ao nível teórico, os conceitos de holismo e cuidar, dominam as conceções subjacentes à formação dos estudantes, é o desempenho e treino de procedimentos técnico-instrumentais que é privilegiado, com os ensinos clínicos a ocorrerem maioritariamente em contextos hospitalares. A aposta nos cuidados de saúde comunitários tem um menor impacto ao nível dos currículos, quer em termos teóricos quer práticos (Correia, 2008). As RS construídas pelos estudantes expressam uma realidade simbólica, não apreensível numa primeira aproximação, mas com capacidade de mobilizar a realidade gerando e orientando comportamentos e atitudes (Formozo e Oliveira, 2010). As RS marcam o processo de construção da identidade profissional e as opções futuras pelo contexto de trabalho. Objetivos: Identificar e comparar as RS dos cuidados hospitalares e comunitários em estudantes de enfermagem do 1º e 4º ano. Metodologia: Pesquisa qualitativa orientada pela Teoria das Representações Sociais. Amostra constituída por 132 estudantes do CLE da ESESJDUE, 71 do 1º ano e 61 do 4º ano. Utilizou-se um questionário em que eram apresentados dois estímulos indutores, com recurso à técnica de Associação Livre de Palavras. Foi realizada a análise no Software IRaMuTeQ.. Salvaguardados todos os aspetos éticos relativos a estudos com seres humanos. Resultados: A partir de matrizes cruzando segmentos de texto e palavras, aplicou-se o método da Classificação Hierárquica Descendente e obtivemos 4 classes. A classe 2, remete para os cuidados hospitalares e as classes 1, 3 e 4, para um conjunto de cuidados inerentes ao processo de cuidar os utentes. Na classe 1 a palavra central é ajuda, seguida de bem-estar, cuidado e sociedade, na classe 2 é enfermeiro seguida de médicos, internamento e recurso, na classe 3 é tratamento, seguida de vacina, comunicar e rastreio e na classe 4 é ensino, seguida de urgência, prevenção e promoção. Os dois grandes eixos organizadores da RS são enfermeiro, doença e tratamento, no núcleo central – cuidados hospitalares. Na nuvem de palavras, das mais evocadas destaca-se enfermeiro, doença, tratamento, prevenção, cuidado e ajuda. Conclusões: As RS dos estudantes estruturam-se em torno do papel central do enfermeiro no processo de cuidar. São os cuidados mais próximos da intervenção hospitalar que assumem destaque e posicionam o enfermeiro no centro do processo, sendo a partir daí que se concetualizam os cuidados ao doente, através do tratamento, prevenção, cuidado e ajuda. Salienta-se que as RS remetem para a importância social e especificidade do papel do enfermeiro na sociedade, evidenciados por termos como responsabilidade, ensino, promoção, educar ou apoio. Referências Bibliográficas Brito A. M. R., et al. (2011). Representações sociais de discentes de graduação em enfermagem sobre “ser enfermeiro”. Rev Bras Enferm, Brasilia 2011 mai-jun; 64(3): 527-35. Correia, Raquel (2008). Enfermeiros recém-formados e Cuidados de Saúde Comunitários: as lógicas subjacentes à escolha. Sísifo. Revista de Ciências da Educação, 05, pp. 45-58. Consultado em [maio, 2014] em http://sisifo.fpce.ul.pt Formozo GA, Oliveira DC. (2010). “Representações sociais do cuidado prestado aos pacientes soropositivos ao HIV”Rev Bras Enferm, mar-abr; 63(2): 230-7

Palisada flagellifera (Ceramiales, Rhodophyta) from the Canary Islands, Spain: a new record for the eastern Atlantic Ocean based on morphological and molecular evidence

Palisada flagellifera (Ceramiales, Rhodophyta) is recorded for the first time in the eastern Atlantic Ocean off Tenerife, La Gomera, La Palma and Fuerteventura, Canary Islands, Spain. The specimens were collected in 2006-2009 growing from the lower intertidal to subtidal zones to 2 m depth at sites exposed to wave action. The species possesses a palisade-like arrangement of cortical cells in cross section, lacks secondary pit connections between them, and has tetrasporangia produced by three fertile pericentral cells (the third and the fourth additional and the second that becomes fertile), and a right-angled arrangement of tetrasporangia. Gametangia were not observed. The phylogenetic relationships were inferred by analyses of the chloroplast-encoded rbcL gene sequences from 46 taxa. The Canarian and Brazilian P. flagellifera specimens formed a highly supported clade with a low level of genetic variation in the rbcL sequences (0.02-0.04%), confirming that they are the same taxonomic entity. This study expands the geographical distribution of P. flagellifera to the eastern Atlantic Ocean.

Evidence for the conspecificity of Palisada papillosa with P. perforata (Ceramiales, Rhodophyta) from the western and eastern Atlantic Ocean on the basis of morphological and molecular analyses

Morphological and molecular studies were carried out on Palisada papillosa and P. perforata from the Canary Islands (type locality of P. perforata), Mexico and Brazil. The two species have been distinguished by features of their external morphology such as size and degree of compactness of the thalli, presence or absence of arcuate branches, branching pattern and basal system. A detailed morphological comparison between these taxa showed that none of the vegetative anatomical or reproductive characters was sufficient to separate these species. The presence or absence of cortical cells in a palisade-like arrangement, also previously used to. distinguish these species, is not applicable. The species present all characters typical of the genus, and both share production of the first pericentral cell underneath the basal cell of the trichoblast, production of two fertile pericentral cells (the second and the third additional, the first remaining sterile), spermatangial branches produced from one of two laterals on the suprabasal cell of trichoblasts, and the procarpbearing segment with four pericentral cells. Details of the procarp are described for the species for the first time. The phylogenetic position of these species was inferred by analysis of the chloroplast-encoded rbcL gene sequences from 39 taxa, using one other Rhodomelacean taxon and two Ceramiaceae as outgroups. Relationships within the clade formed by P. papillosa and P. perforata have not been resolved due to the low level of genetic variation in their rbcL sequences (0-0.4%). Considering this and the morphological similarities, we conclude that P. papillosa is a taxonomic synonym of P. perforata. The phylogenetic analyses also supported the nomenclatural transfer of two species of Chondrophycus to Palisada, namely, P. patentiramea (Montagne) Cassano, Senties, Gil-Rodriguez & M.T. Fujii comb. nov. and P. thuyoides (Kutzing) Cassano, Senties, Gil-Rodriguez & M.T. Fujii comb. nov.

Lipid, fatty acid, protein, amino acid and ash contents in four Brazilian red algae species

Four species of marine benthic algae (Laurencia filiformis, L. intricata, Gracilaria domingensis and G. birdiae) that belong to the phylum Rhodophyta were collected in Espirito Santo State, Brazil and investigated concerning their biochemical composition (fatty acid, total lipid, soluble proteins, amino acid and ash). The total content of lipid (% dry weight) ranged from 1.1% to 6.2%: fatty acid from 0.7% to 1.0%: soluble protein from 4.6% to 18.3%, amino acid from 6.7% to 11.3% and ash from 22.5% to 38.4%. judging from their composition, the four species of algae appear to be potential sources of dietary proteins, amino acids, lipids and essential fatty acids for humans and animals. (C) 2009 Elsevier Ltd. All rights reserved.

Morphological and molecular evidences within Osmundea (Ceramiales, Rhodophyta) from the Canary Islands, eastern Atlantic Ocean

The genus Osmundea is a strongly supported monophyletic group within the Laurencia complex and shows a disjunct distribution occurring in the North-East and South-West Pacific, the Indian and Atlantic oceans and the Mediterranean Sea. Its phenotypic plasticity on the Canary Islands may be the result of the high ecological variability partially due to the particular oceanographic characteristics in this region. The combination of molecular analyses based on the comparison of the chloroplast-encoded rbcL sequences and morphological data allowed us to delimit three distinct taxa from the coasts of the Canarian Archipelago: Osmundea pinnatifida, Osmundea truncata and an unidentified species, Osmundea sp. Moreover, the high value of genetic divergence between Osmundea sp. and the rest of the Osmundea species suggests that this taxon should be assigned to a new species within the Osmundea genus. Occurrence of O. hybrida and O. oederi (synonym: O. ramosissima) has not been confirmed. Our results also suggest a possibly questionable record of the taxa O. hybrida and O. oederi on the Canary Islands.

Ecología y estatus trófico del erizo de mar Diadema antillarum (Philippi, 1845) en los fondos rocosos de las Islas Canarias (Gran Canaria, España)

La explosión demográfica de erizo Diadema antillarum en los ecosistemas sumergidos rocosos del litoral canario está provocando una intensa desertización, generando los popularmente conocidos como fondos de “blanquizales” debido al color blanco que adquiere el recubrimiento calcáreo. Se analizaron los parámetros morfométricos, de densidad poblacional, ecología trófica e interacción específica de la especie de erizo D. antillarum (Philippi, 1845) durante los años 2005, 2006 y 2007 en los fondos rocosos de la isla de Gran Canaria, Islas Canarias, España. Se evaluaron cuatro blanquizales con diferente orientación geográfica y con características bióticas y abióticas distintas, lo que permitió analizar el papel trófico de D. antillarum bajo diferentes condiciones; además de la evaluación de la biomasa de las especies algales halladas en los fondos rocosos donde habita la especie. El estudio hace un especial énfasis en la evaluación de la distribución, discriminación y selección de las diversas fuentes algales consumidas por Diadema antillarum a través de un seguimiento de la asimilación de los productores primarios por los consumidores, mediante el uso de los isótopos estables 13C y 15N Los resultados no mostraron una variación estacional de la morfometría de D. antillarum. Sin embargo, si existe una variación respecto al tamaño del erizo con la profundidad. La especie mostró una disminución de su tamaño cuanto mayor era la profundidad. Asimismo los resultados exhibieron una correlación negativa entre la densidad poblacional de D. antillarum y el tamaño del erizo. Hay una clara tendencia a hallar las tallas pequeñas de erizos conforme aumenta la maduración o desarrollo de los blanquizales. Se encuentran tallas menores cuando la densidad de erizos supera los 5 erizos • m-2. La mayor densidad promedio encontrada en este estudio fue de 12, 83 erizos • m-2 y la talla menor fue de un diámetro de caparazón menor a 2 cm y un ancho de la linterna de Aristóteles de 0,8 cm; la categoría de diámetro de caparazón más abundante fue la comprendida en el rango de 3,5-5,4 cm. Las firmas isotópicas de la fuentes algales y del músculo de D. antillarum mediante el uso de modelos de mezcla permitieron concluir que en términos generales el género Laurencia resultó un constituyente principal en la dieta de D. antillarum en los diferentes blanquizales; los géneros Colpomenia, Padina, Sargassum, Hypnea, y Jania son constituyentes importantes en la dieta de D. antillarum cuando habita en sustratos de blanquizales desarrollados (maduros), de la misma forma que Dictyota, Zonaria, Liagora, Lobophora, y Stypocaulon constituyen fuentes importantes en los blanquizales menos desarrollados (inmaduros), mostrando un alto grado de solapamiento de fuentes. D. antillarum presentó una asimilación diferencial, independientemente de la disponibilidad del alimento. La dieta de D. antillarum refleja una composición algal específica dependiendo de la etapa de maduración del blanquizal El estudio proporciona una herramienta cuantitativa que permite separar ambientes diferentes - hábitats que experimentan diferentes grados de perturbación- a través de la evaluación de una asimilación diferencial de las algas por parte de D. antillarum.

Concerning the proposed structure of (+)-laurobtusol: Spectral discrepancies with synthetic, racemic Stereoisomers

Laurobtusol, a minor metabolite from Laurencia obtusa, had been assigned constitution 1 and relative stereochemistry, 2. However, several stereoisomers of this novel, cyclopropane-containing system 1 have now been synthesized and spectral correspondence between the synthesized isomers and laurobtusol is lacking.

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.