GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 2005-2009  (37)
  • 1990-1994  (6)
Document type
Keywords
Language
Years
Year
  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Deep sea corals. ; Electronic books.
    Description / Table of Contents: This broad-ranging treatment is the first to synthesise current understanding of all types of cold-water coral worldwide. Covering ecology, biology, palaeontology and geology, the text is enhanced by an extensive glossary, online resources, and a unique collection of colour photographs and illustrations of corals and the habitats they form.
    Type of Medium: Online Resource
    Pages: 1 online resource (368 pages)
    Edition: 1st ed.
    ISBN: 9780511539329
    DDC: 593.6/1779
    Language: English
    Note: Cover -- Half-title -- Title -- Copyright -- Contents -- Topic boxes and Case studies -- Preface -- Acknowledgements -- 1 History and research approaches -- 1.1 History -- 1.1.1 Early history and taxonomy -- 1.1.2 Pioneering deep-sea expeditions -- 1.1.3 The modern era begins -- 1.2 Research approaches -- 1.2.1 Exploration -- 1.2.2 Habitat mapping -- 1.2.3 Collecting samples -- 1.2.4 Monitoring -- 1.2.5 Technologies for the future -- 2 Cold-water corals -- 2.1 Ecological categorisation of corals -- 2.2 The five cold-water coral taxa -- 2.2.1 Scleractinia -- 2.2.2 Zoanthidae -- 2.2.3 Antipatharia -- 2.2.4 Octocorallia -- 2.2.5 Stylasteridae -- 2.3 Environmental controls on cold-water coral distribution -- 2.4 Global patterns of cold-water scleractinian diversity -- 2.5 Molecular phylogeny of cold-water corals -- 2.6 Linkages and connectivity -- 3 Biology -- 3.1 Anatomy -- 3.2 Morphology -- 3.3 Food supply and nutrition -- 3.3.1 Gas seeps and the 'hydraulic theory' -- 3.3.2 Hydrography -- 3.3.3 Food particles -- 3.4 Growth rates -- 3.4.1 Growth bands and chronologies -- 3.4.2 Longevity and carbon sources -- 3.5 Ecophysiology -- 3.5.1 Respiratory physiology -- 3.5.2 Excretion and osmotic balance -- 3.5.3 Nervous and endocrine control -- 3.6 Reproduction -- 3.7 Larval biology and dispersal -- 4 Reefs and mounds -- 4.1 Reef initiation and development -- 4.2 Reef sedimentation -- 4.2.1 Matrix sediment and deposits -- 4.2.2 Deposit-based cold-water coral reef classification -- 4.3 Defining coral carbonate mounds -- 4.4 Mound development -- 4.4.1 Mound initiation -- 4.4.2 Mound growth -- 4.4.3 Accumulation rates -- 4.4.4 Climatic controls on mound growth -- 4.4.5 Diagenetic processes -- 4.4.6 Late-stage mound development and burial -- 4.5 Coral carbonate mound morphology -- 4.5.1 Mound shape -- 4.5.2 Mound dimensions. , 4.6 Global distribution of coral carbonate mounds -- 5 Habitats and ecology -- 5.1 Habitats -- 5.1.1 Reefs -- 5.1.2 Gorgonian forests and coral gardens -- 5.2 Biodiversity -- 5.2.1 Megafauna and macrofauna -- 5.2.2 Meiofauna -- 5.2.3 Microbial diversity -- 5.3 Seamounts, endemism and refugia -- 5.4 Species interactions -- 5.4.1 Symbiosis -- 5.5 Fish assemblages -- 5.6 Predictive mapping -- 6 Palaeontology -- 6.1 Triassic dawn -- 6.2 Fossil record of cold-water corals -- 6.2.1 Dendrophylliidae -- 6.2.2 Oculinidae -- 6.2.3 Caryophylliidae -- 6.3 Taphonomy -- 6.3.1 Growth of the coral framework -- 6.3.2 Breakdown of the coral framework -- 6.4 Preservation of the coral-associated fauna -- 6.4.1 Foraminifera -- 6.4.2 Porifera -- 6.4.3 Cnidaria -- 6.4.4 Annelida -- 6.4.5 Mollusca -- 6.4.6 Crustacea -- 6.4.7 Echinodermata -- 6.4.8 Bryozoa -- 6.4.9 Other groups -- 7 Corals as archives -- 7.1 Biomineralisation -- 7.1.1 Coral calcification -- 7.1.2 Vital effects -- 7.2 Temperature records -- 7.3 Water-mass history -- 7.4 Pollution and nutrient records -- 8 Impacts and conservation -- 8.1 Impacts -- 8.1.1 Fishing -- 8.1.2 Oil and gas -- 8.1.3 Mining -- 8.1.4 Climate change and ocean acidification -- 8.1.5 Coral collection -- 8.1.6 Other threats -- 8.2 Conservation -- 8.2.1 Protected areas -- 8.2.2 Monitoring -- 8.2.3 The high seas -- 8.2.4 Stewardship -- Glossary -- References -- Index.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Deep-sea ecology -- Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (1273 pages)
    Edition: 1st ed.
    ISBN: 9783540276739
    Series Statement: Erlangen Earth Conference Series
    DDC: 577.7/89
    Language: English
    Note: Intro -- CONTENTS -- Foreword -- Preface -- Contributors -- I The paleoenvironmental context -- II Distribution -- III Mapping -- IV Exogenic and endogenic controls -- V Coral Biology -- VI Diversity -- VII Environmental Archive -- VIII Conservation -- Index.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Keywords: Corals Congresses ; Deep sea ecology Congresses ; Coral reef ecology Congresses ; Aufsatzsammlung ; Konferenzschrift ; Kaltwasser ; Korallenriff ; Ökosystem ; Kaltwassersphäre ; Lophelia
    Description / Table of Contents: Following the exciting exploration of hot vent and cold seep ecosystems, the rediscovery of cold- and deep-water coral ecosystems in our oceans with high-technology instrumentation is currently another hot topic in multidisciplinary marine research. Conventionally, coral reefs are regarded as being restricted to warm and well-illuminated tropical seas, but not with cold and dark waters of the higher latitudes. However, ongoing scientific missions currently shed light on the global significance of this overlooked ecosystem. Cold-water coral ecosystems are involved in the formation of large seabed structures such as reefs and giant carbonate mounds, and they represent unexploited paleo-environmental archives of Earth history. Like their tropical cousins, cold-water coral ecosystems harbour rich species diversity. Despite the great water depths, commercial interests more and more overlap with the coral occurrences. Damage created by human activities is already taking place worldwide and caused severe damage to the vulnerable ecosystem. The current key institutions involved in cold-water coral research have contributed 65 state-of-the-art articles covering the disciplines of geology and biology
    Type of Medium: Book
    Pages: XXXII, 1243 S , Ill. (z. T. farb.), graph. Darst., Kt , 270 mm x 193 mm
    ISBN: 9783540241362 , 3540241361
    Series Statement: Erlangen Earth Conference series
    DDC: 577.789
    RVK:
    RVK:
    RVK:
    RVK:
    Language: English
    Note: Index S. [1211] - 1243
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: Online-Ressource (63 S.) , Ill., graph. Darst., Kt.
    Series Statement: Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen 260
    DDC: 550
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    In: Earth and planetary science letters, Amsterdam [u.a.] : Elsevier, 1966, 269(2008), 3/4, Seite 570-575, 1385-013X
    In: volume:269
    In: year:2008
    In: number:3/4
    In: pages:570-575
    Type of Medium: Online Resource
    ISSN: 1385-013X
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    In: Oceanography, Rockville, MD : The Oceanography Society, 1988, 22(2009), 1, Seite 58-74, 2377-617X
    In: volume:22
    In: year:2009
    In: number:1
    In: pages:58-74
    Description / Table of Contents: White coral communities consist of scleractinian corals that thrive in the ocean’s bathyal depths (~ 2004000 m). In the Atlantic Ocean, white corals are known to form complex, three-dimensional structures on the seabed that attract vast amounts of other organisms, accumulate suspended detritus, and influence the local hydrodynamic flow field. These attributes coincide with what we generally describe as a coral reef. With time, environmental change causes decline of the framework-constructing corals; this is followed by erosion of the reef sequence or its draping with noncoral-related deposits. After several such sequences, the structures are known as coral carbonate mounds, which can grow as high as 350 m. Both bathyal white coral reefs and mounds are widely distributed in the Atlantic Ocean and adjacent marginal seas, such as the Gulf of Mexico. The Mediterranean Sea, however, known for its richness of fossil white coral communities exposed in land outcrops, harbors very few extant coral communities. The HERMES project extended its study sites deep into the Mediterranean with state-of-the-art mapping and visualization technology. By doing so, many previously unknown coral sites were discovered during inspections of Mediterranean narrow shelves, canyon walls, escarpments, and seamounts by remotely operated vehicles. Such shelf and continental margin settings are characteristic of the dynamic margins of the Mediterranean Sea and contrast significantly with the much broader shelves of the Atlantic Ocean. This paper reports on a HERMES cruise that was dedicated to exploring these rough submarine topographies in search of white coral communities in the central Mediterranean, and re-evaluates the general perception of the assumed paucity of white corals in this sea.
    Type of Medium: Online Resource
    Pages: Ill., graph. Darst
    ISSN: 2377-617X
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    In: Von Agrar- bis Wirtschaftswissenschaften: alle über einen Leisten?, Hannover : Wiss. Komm. Niedersachsen, 2009, (2009), Seite 55-57
    In: year:2009
    In: pages:55-57
    Type of Medium: Article
    Language: German
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Keywords: Hochschulschrift ; Nordnorwegen ; Riff ; Kalkalgen ; Eustatische Meeresspiegelschwankung
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (215 Seiten = 21 MB) , Illustrationen, Graphen, Karten
    Edition: Online-Ausgabe
    Language: German
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2023-08-25
    Description: Riffe haben seit den Arbeiten DARWINS nichts von ihrer Faszination als Objekte biologischer und geologischer Forschung eingebüßt. So widmet sich der DFG-Schwerpunkt "Riff-Evolution und Kreide-Sedimentation" der Erforschung von Steuerungsprozessen in diesen bedeutenden Ökosystemen an ausgewählten fossilen und rezenten Fallbeispielen. Das Riff, das in dieser Untersuchung vorgestellt wird, wächst in einem vor wenigen Jahrtausenden noch vergletscherten Gebiet in Nordnorwegen nördlich des 70° Breitengrades. Es stellt sich daher vorrangig die Frage nach dem Faktorengefüge, welches eine Riftbildung unter hochboreal-subarktischen klimatischen Bedingungen ermöglicht. Die Beantwortung dieser wichtigen Frage umschlieBt eine Analyse von geologischen und biologischen Prozessen, die sich in unterschiedlichen zeitlichen Maßstaben abspielen: von den intra-annualen Zyklen (Fortpflanzung, Stürme, etc.) bis hin zu MILANKOVITCH-Zyklen in der Größenordnung von 104 bis 105 Jahren. Das untersuchte Riff hat eine Ausdehnung von 125000m2 und existiert seit mindestens 200 Jahren. Obwohl die Kalkalgen nur ca. einen Millimeter pro Jahr wachsen, liegen die Karbonatproduktionsraten von durchschnittlich 1400g m-2 Calziumkarbonat pro Jahr in etwa in der Größenordnung tropischer Kalkalgen. Die Ursache liegt im außerordentlich hohen Konkurrenzvermögen der langsamwachsenden Kalkalgen gegenüber anderen schnellwüchsigen sessilen Karbonatproduzenten, z.B. Balaniden, Bryozoen, Serpuliden und Spirorbiden. Der weitgehende Ausschluß dieser sessilen Invertebraten von der lebenden Kalkalgenoberfläche führt zu einem geringdiversen, jedoch außerordentlich dicht besiedelten Kalkalgen-Ökosystem. Die Steuerung ist das Ergebnis komplexer co-evolutiver Wechselwirkungen zwischen Kalkalgen, Bakterien und den Larven herbivorer Organismen. Diageneseprozesse beginnen in vivo, beschränken sich jedoch auf die Zementation intrapartikularer Zellhohlraume der Algenthalli. Dadurch erfahren die Algen frühzeitig eine interne Stabilisierung. Neben der Bioerosion kontrollieren Stürme das Sedimentationsgeschehen im Riff. Die-Riff-assoziierten Sedimentstrukturen lassen sich auf Sturmereignisse zurückführen. Dabei entstehen in Abhängigkeit von der Küstentopographie charakteristische sedimentäre Fazies. Sturmumlagerungen vor einer geschlossenen Küstenlinie erzeugen parallele Fazieszonen um das Riff. Die Masse des umgelagerten Riffschutts wandert in Richtung Strand. Algen-Bioherme in einem Sund weisen eine einsinnig gerichtete Faziesabfolge auf. Hier kommt es zu episodiscben Dislokationen bis in die Fjordtröge. Bedingt durch die glazio-isostatische Hebung Fennoskandiens erlauben großflächige Landaufschlüsse eine hohe zeitliche Auflösung der Etablierung der Karbonatfazies nach dem Ende des letzten Glazials. Karbonatsedimente sind seit dem Atlantikum (8000-5000 J.v.h.) vorhanden. Die Karbonatproduktion wurde auch im Holozän von Kalkalgen dominiert. Jedoch belegen die 14C-Alter autochthoner subtidaler Kalkalgen-Bivalven-Gemeinschaften episodische Produktionsphasen um 6000 bis 5500 J.v.h und 4800-3800 J.v.h. In diese Zeitintervalle fallen auch bedeutende Umlagerungsereignisse, die durch weitläufige Strandwall-Ablagerungen dokumentiert sind. Jüngere Strandwälle, die den sukzessiven Rückzug des Meeres von den sich hebenden Küstenplattformen belegen, wurden vor 3400-2600 J.v.h. und 1800-900 J.v.h. angelegt. Das Auftreten der Produktionsphasen der subtidalen Karbonatproduzenten und die massiven Umlagerungsphasen stehen im Einklang mit den hochfrequenten Meeresspiegelfluktuationen, die seit 6000 Jahren im Untersuchungsgebiet nachzuweisen sind. Biogene Karbonatproduktion durch Kalkalgen ist immer dann bedeutend, wenn die insgesamt regressive Tendenz, bedingt durch die Hebung des Untergrundes, durch eustatische Transgressionen kompensiert wird. In diesen Zeiten herrschen 'stabile' hydrographische Umweltbedingungen hinsichtlich des Meeresspiegelniveaus vor. Während dieser Phasen können Sturmereignisse große Strandwallsysteme im Intertidal aufbauen. Die Untersuchungen zeigen, daß bereits wenige Tausend Jahre nach dem Rückzug der Gletscher bedeutende Karbonatproduktion bis hin zur Bildung von Riffen einsetzen kann.
    Type: Thesis , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    Springer
    In:  Facies, 29 (1). pp. 133-148.
    Publication Date: 2016-04-15
    Description: In the subtropical belt highly productive ecosystems are formed by coral reefs in oligotrophic seas. Towards more eutrophic conditions, coral reefs diminish and are subsequently replaced by highly productive kelp forests. In high latitudes framework constructing carbonate production is enhanced by the growth of branching coralline algae which predominantly generate maerl-type deposits. On a global view, these coralline algal ecosystems show an island-like distribution pattern within the phaeophytic kelp belt. Compared to kelp ecosystems, coralline-algaldominated ecosystems have low rates of productivity. Therefore, it is reasonable to seek the pronounced competitive value of the extremely slow-growing corallines. Due to their low annual growth increment, the coralline algae studied are very endangered by abiotic physical disturbances and by overgrowth of rapidly growing filamentous algae or sessile invertebrates. To overcome fouling pressure and storm-triggered physical disturbances, coralline algae thrive well in wave-sheltered headlands or skerry areas and generate characteristic ‘denuded areas’ by intense herbivory. This general distributional pattern is also true for high-boreal to subarctic coralline algal bioherms in northern Norway. Such a complex biological feedback maintains a high potential of self-regulation or self-organization in the algal reef bioherms. The different proponents involved in feedback processes include bacterial colonization, diatom microfouling and selective induction of larval metamorphosis. The negative impact of diatom microfouling and the important role of herbivores are relevant activities in the feedback system on a microscopic scale. Macroscopically, intense herbivory on coralline algae create denuded conditions, which are a widespread phenomenon in coralline algal ecosystems.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...