Neuweiler, Fritz

[["dc.bibliographiccitation.firstpage","851"],["dc.bibliographiccitation.issue","9"],["dc.bibliographiccitation.journal","Geology"],["dc.bibliographiccitation.lastpage","854"],["dc.bibliographiccitation.volume","28"],["dc.contributor.author","Neuweiler, Fritz"],["dc.contributor.author","Rutsch, M."],["dc.contributor.author","Geipel, G."],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Heise, K. H."],["dc.date.accessioned","2018-11-07T10:30:38Z"],["dc.date.available","2018-11-07T10:30:38Z"],["dc.date.issued","2000"],["dc.description.abstract","Albian carbonate mud-mound limestones exposed near Iraneta, northern Spain, show a fabric- and particle-specific fluorescence. Intense fluorescence is restricted to in situ precipitated microcrystalline (automicritic) fabrics, calcified demosponges, and coralline sponges. Intermediate intensity derives from micritized bioclasts, pellets, and a rim of marine bladed cement. Most invertebrate skeletons, late-diagenetic equant cement, and crosscutting zones of dolomitization are weakly to nonfluorescent. Internal microcrystalline sediment (allomicrite) and red algae debris have variable fluorescence. Correlation between rock fluorescence and soluble humic substances was evaluated from 3 g of automicrite, allomicrite, and cement. Time-resolved laser-induced fluorescence spectroscopy (TRLFS) with ultra-short pulses on two extracrystalline fractions (NaOH-soluble) and two intracrystalline fractions (HCl-soluble and NaOH-soluble) showed that most of the soluble humic substances of automicrite are within the crystals; but conversely, are significantly enriched on outer surfaces of allomicrite. Spar cement is close to detection limits. Fluorescence lifetimes are in the range of 0.5-2 ns and 3.5-6 ns. We conclude that precipitation of automicrite took place during oxidative organic matter diagenesis, i.e., during condensation reactions of degradation products of marine biopolymers. By contrast, allomicrite formed by skeletal breakdown followed by ingestion, organic coating, and reingestion during deposit feeding. A humic-substance-based model of marine polymer gels represents a new approach for the understanding of ancient polygenetic carbonate muds, so typical of Phanerozoic mud-mounds in deeper water settings."],["dc.identifier.doi","10.1130/0091-7613(2000)028<0851:SHSFIS>2.3.CO;2"],["dc.identifier.isi","000089269100021"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/43909"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0091-7613"],["dc.title","Soluble humic substances from in situ precipitated microcrystalline calcium carbonate, internal sediment, and spar cement in a Cretaceous carbonate mud-mound"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","273"],["dc.bibliographiccitation.journal","Berliner geowissenschaftliche Abhandlungen"],["dc.bibliographiccitation.lastpage","293"],["dc.bibliographiccitation.seriesnr","3"],["dc.bibliographiccitation.volume","3"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Neuweiler, Fritz"],["dc.contributor.editor","Kohring, Rolf"],["dc.date.accessioned","2019-07-10T08:12:30Z"],["dc.date.available","2019-07-10T08:12:30Z"],["dc.date.issued","1992"],["dc.description.abstract","Aus dem Unter-/Mittelalb von Nordspanien wird ein Profil mit bis zu 8 m mächtigen Lithocodium/ Bacinella Boundstones vorgesteUt. Die mikrofaziell-sedimentologische Analyse des Profils crgibt für die Lithocodium/ Bacinella Bänke eine bathymetrische Position vom tieferen Subtidal bis flachsten Subtidal/lntertidal. Die maximale Tiefenposition ist an die photische Zone gebunden, die wiederum durch das Ausmaß toniger Suspensionen beeinflußt wird. Die bathymetrische Obergrenze ist mechanisch kontrolliert (z.B. WeUenenergie, Tidenströme). Lithocodium/Bacinella ist zusammen mit anderen Algen/Mikroben ein charakteristischer Bestandteil thrombolithischer Mud Mounds (z.B. Gandara Mound). Die funktionelle Rolle von Lithocodium/Bacinella bei der Mud Mound Genese umfaßt Baffling und Binding, AutomikritProduktion durch Kalzifizierung innerhalb organischer Schleimhüllen und eine Mikritproduktion über intensive Bohraktivitäten an eingelagerten karbonatischen Hartteilen. Das massenhafte Auftreten von Lithocodillm/ Bacinella und diversen Algen/Mikroben kann mit einer längerfristigen Eutrophierung des Lebensraumes oder mit Schwankungen der Karbonat-Alkalinät des Meerwassers erklärt werden."],["dc.description.abstract","A section including Lithocodium/ Bacinella boundstones with a thickness of up to 8 m is reported from the Lower /Middle Albian of northern Spain. According to microfacies and sedimentological analyses the bathymetric position of the Lithocodium/ Bacinella banks ranges from deeper subtidal to shaUowest subtidal/intertidal conditions. The maximum depth is related to the photic zone, which ,itself is controled by the amount of muddy suspension. The upper bathymetric limit is mechanically defin'ed and corresponds to increased depositional energy (i.e. waves and tidal currents). Together with other algae and microbes Lithocodium/ Bacinella is a major constituent of thrombolitic mud mounds (Gandara mound). In the context of mud mound genesis the functional role of Lithocodium/ Bacinella includes baffling and binding, the production of micrite via the calcification inside of mucilagenous sheaths, and via intensive boring activities upon and inside of skeletal hardparts. The mass occurrence of Lithocodium/ Bacinella with associated algae and microbes may be explained by a longer ranging eutrophism of the environment or by shifts in seawater carbonate alkalinity."],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","50213349x"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2172"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60942"],["dc.language.iso","de"],["dc.notes.intern","Migrated from goescholar"],["dc.publisher","Fachber. Geowissenschaften"],["dc.publisher.place","Berlin"],["dc.relation.crisseries","Berliner geowissenschaftliche Abhandlungen. Reihe E, Paläobiologie"],["dc.relation.ispartof","Miscellanea palaeontologica"],["dc.relation.ispartofseries","Berliner geowissenschaftliche Abhandlungen. Reihe E;3"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Karbonatbänke mit Lithocodium aggregatum Elliott, Bacinella irregularis Radoicic ; Paläobathymetrie, Paläoökologie und stratigraphisches Äquivalent zu thrombolithischen Mud Mounds"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","338"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Terra Nova"],["dc.bibliographiccitation.lastpage","346"],["dc.bibliographiccitation.volume","13"],["dc.contributor.author","Neuweiler, F."],["dc.contributor.author","Bourque, P. A."],["dc.contributor.author","Boulvain, F."],["dc.date.accessioned","2018-11-07T08:38:00Z"],["dc.date.available","2018-11-07T08:38:00Z"],["dc.date.issued","2001"],["dc.description.abstract","The sedimentary-diagenetic structure stromatactis is wide-spread in Palaeozoic spiculitic carbonate mud mounds, but occurs only sporadically in Mesozoic sponge carbonate mud mounds. Comparative analysis of Palaeozoic and Mesozoic stromatactis limestones suggests that this variation results from the degree of siliceous sponge skeletal rigidity and the amount of internal sediment accumulation in the original cavity network. Partial to entire filling by internal sediment resulted in a continuum, from a small amount of internal sediment and large amount of cement (stromatactis, common in the Palaeozoic), to only internal sediments (aborted stromatactis, common in the Mesozoic). These observations match independent lines of evidence concerning the siliceous sponge evolution and sediment recycling (e.g. bioerosion) across the Palaeozoic to Mesozoic biotic revolution."],["dc.identifier.doi","10.1046/j.1365-3121.2001.00367.x"],["dc.identifier.isi","173564900005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/18672"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Blackwell Publishing Ltd"],["dc.relation.issn","0954-4879"],["dc.title","Why is stromatactis so rare in Mesozoic carbonate mud mounds?"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","130"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","146"],["dc.bibliographiccitation.volume","94"],["dc.contributor.author","Neuweiler, F."],["dc.contributor.author","Bernoulli, D."],["dc.date.accessioned","2018-11-07T08:28:16Z"],["dc.date.available","2018-11-07T08:28:16Z"],["dc.date.issued","2005"],["dc.description.abstract","The Broccatello lithological unit (Lower Jurassic, Hettangian to lower parts of Upper Sinemurian) near the village of Arzo (southern Alps, southern Switzerland) is a mound-shaped carbonate deposit that contains patches of red stromatactis limestone. Within the largely bioclastic Broccatello unit, the stromatactis limestone is distinguished by its early-diagenetic cavity system, a relatively fine-grained texture, and an in-situ assemblage of calcified siliceous sponges (various demosponges and hexactinellids). A complex shallow subsurface diagenetic pathway can be reconstructed from sediment petrography in combination with comparative geochemical analysis (carbon and oxygen isotopes; trace and rare earth elements, REE + Y). This pathway includes organic matter transformation, aragonite and skeletal opal dissolution, patchy calcification and lithification, sediment shrinkage, sagging and collapse, partial REE remobilization, and multiple sediment infiltration. These processes occurred under normal-marine, essentially oxic conditions and were independent from local, recurring syn-sedimentary faulting. It is concluded that the stromatactis results from a combination of calcite mineral authigenesis and syneresis-type deformation. The natural stromatactis phenomenon may thus be best explained by maturation processes of particulate polymer gels expected to form in fine-grained carbonate sediments in the shallow subsurface. Conditions favorable for the evolution of stromatactis appear to be particularly frequent during drowning of tropical or subtropical carbonate platforms."],["dc.identifier.doi","10.1007/s00531-004-0442-3"],["dc.identifier.isi","000227047800012"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/16381"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1437-3262"],["dc.relation.issn","1437-3254"],["dc.title","Mesozoic (Lower Jurassic) red stromatactis limestones from the Southern Alps (Arzo, Switzerland): calcite mineral authigenesis and syneresis-type deformation"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.volume","94"],["dc.contributor.author","Neuweiler, F."],["dc.contributor.author","Bernoulli, D."],["dc.date.accessioned","2018-11-07T11:11:22Z"],["dc.date.available","2018-11-07T11:11:22Z"],["dc.date.issued","2005"],["dc.format.extent","317"],["dc.identifier.doi","10.1007/s00531-005-0485-0"],["dc.identifier.isi","000228539200013"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53414"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1437-3262"],["dc.relation.issn","1437-3254"],["dc.title","Mesozoic (Lower Jurassic) red stromatactis limestones from the Southern Alps (Arzo, Switzerland): calcite mineral authigenesis and syneresis-type deformation (vol 94, pg 130, 2004)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","41"],["dc.bibliographiccitation.journal","Facies"],["dc.bibliographiccitation.lastpage","54"],["dc.bibliographiccitation.volume","29"],["dc.contributor.author","Keupp, Helmut"],["dc.contributor.author","Jenisch, Angela"],["dc.contributor.author","Herrmann, Regina"],["dc.contributor.author","Neuweiler, Fritz"],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2008-10-29T20:05:05Z"],["dc.date.accessioned","2021-10-27T13:13:57Z"],["dc.date.available","2008-10-29T20:05:05Z"],["dc.date.available","2021-10-27T13:13:57Z"],["dc.date.issued","1993"],["dc.description.abstract","Morphological and geochemical comparisons between modern cryptic microbialites from Lizard Island/Great Barrier Reef and fossil counterparts in the Upper Jurassic (Southern Germany, Dobrogea/Romania) and late Lower Cretaceous (Aptian/ Albian from Cantabria/Spain) spongiolitic environments show that there are common factors controlling the crust formations mostly independent of light despite of diverging (paleo-) oceanographic positions as well as relationships of competitors. Factors such as increased alkalinity ,oligotrophy, and reduced allochthonous deposition are of major importance. Thrombolitic microbialites are interpreted as biologically induced and therefore calcified in isotopic equilibrium with the surrounding sea water. Corresponding with shallowing upward cycles, microbial mats which produce stromatolitic peloidal crusts become more important. Different biomarkers are introduced for the first time extracted and analyzed from spongiolitic limes tones ofLower Kimmeridgian age from Southern Germany."],["dc.format.mimetype","application/pdf"],["dc.identifier.doi","10.1007/BF02536916"],["dc.identifier.ppn","502136790"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2191"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/91820"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Microbial carbonate crusts - a key to the environmental analysis of fossil spongiolites?"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","837"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Sedimentology"],["dc.bibliographiccitation.lastpage","859"],["dc.bibliographiccitation.volume","46"],["dc.contributor.author","Neuweiler, Fritz"],["dc.contributor.author","Gautret, Pascale"],["dc.contributor.author","Thiel, Volker"],["dc.contributor.author","Lange, Robert"],["dc.contributor.author","Michaelis, Walter"],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2018-07-05T14:05:45Z"],["dc.date.available","2018-07-05T14:05:45Z"],["dc.date.issued","1999"],["dc.description.abstract","The process of organomineralization is increasingly well understood with respect to modern carbonate sediments accumulating adjacent to tropical reef atolls and reef caves. Mineralization related to non-living organic substrates results in autochthonous micrite production (‘automicrites’). ‘Automicrites’ are the main constructive element of Lower Cretaceous (Albian) carbonate mud mounds in northern Spain. These slope mud mounds occur within transgressive and early highstand system tracts encompassing several macrobenthic ecological zones. They are clearly separated from the biocalcifying carbonate factory (Urgonian carbonate platforms), in both space and time. Within these build-ups, most ‘automicrites’ were initially indurated and accreted to form a medium-relief growth framework. ‘Automicrites’ have a uniform, presumably high-Mg-calcite precursor mineralogy. They show an inorganic stable-isotope signature (∂13C around +3·3‰) within the range of early marine cements, and skeletal compounds lacking major vital effects. Epifluorescence microscopy shows that they have facies-specific fluorescence, which is similar to skeletal compounds of Acanthochaetetes, but clearly different from allomicritic sediment and cements, which are mostly non-fluorescent. The EDTA-soluble intracrystalline organic fraction (SIOF) of Albian automicrites shows an amino acid spectrum that is similar to shallow subsurface samples from their modern counterparts. Gel electrophoresis of the SIOF demonstrates an exclusively acidic character, and a mean molecular size range between 20 and 30 kDa. Experiments in vitro (inhibition tests) indicate that the SIOF has a significant Ca2+-binding capacity. Fluorescence and chemical characteristics of SIOF point to a main substance class, such as humic and fulvic acids, compounds that form from pristine organic matter during early diagenesis. Biomarker analyses provide evidence for the crucial role of biodegradation by heterotrophic microorganisms, but no biomarker for cyanobacteria has been found. Primary sources of organic material should have been manifold, including major contributions by metazoans such as sponges. It is concluded that many carbonate mud mounds are essentially organomineralic in origin and that the resulting fabric of polygenetic muds (‘polymuds’) may represent ancestral metazoan reef ecosystems, which possibly originated during the Neoproterozoic."],["dc.identifier.doi","10.1046/j.1365-3091.1999.00255.x"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/15167"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.relation.eissn","0037-0746"],["dc.relation.eissn","1365-3091"],["dc.title","Petrology of Lower Cretaceous carbonate mud mounds (Albian, N. Spain): insights into organomineralic deposits of the geological record"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","243"],["dc.bibliographiccitation.journal","Facies"],["dc.bibliographiccitation.lastpage","264"],["dc.bibliographiccitation.volume","44"],["dc.contributor.author","Neuweiler, F."],["dc.contributor.author","Mehdi, M."],["dc.contributor.author","Wilmsen, M."],["dc.date.accessioned","2018-11-07T09:32:29Z"],["dc.date.available","2018-11-07T09:32:29Z"],["dc.date.issued","2001"],["dc.description.abstract","Liassic sponge mounds of the central High Atlas (Rich area, northern Morocco) have a stratigraphic range from the Lower/Upper Sinemurian boundary interval up to the lower parts of the Lower Pliensbachian (Carixian). The base of Liassic sponge mounds consists of a transgressive discontinuity, i.e., a condensed section of microbioclastic wackestones with firm- and hardgrounds, ferruginous stromatolites, sponge spicules and ammonites. The top of Liassic sponge mounds is an irregular palaeorelief covered by cherty marl-limestone rhythmites, namely hemipelagic spicular wackestones with radiolaria. In the Rich area, section Foum Tillicht, the sponge mound succession has a total thickness of about 250 meters. Within this succession we distinguished between three mound intervals. The lower mound interval shows only small, meter-scale sponge mounds consisting of bound-stones with lyssakine sponges, commensalic Terebella and the problematicum Radiomura. This interval forms a shallowing-upward sequence culminating in a bedded facies with Tubiphytes, calcareous algae (Palaeodasycladus), sponge lithoclasts, coated grains, and thin rims of marine cement. The middle mound interval is aggradational with decametric mounds and distinct thrombolitic textures and reefal cavities. The mound assemblage here consists of hexactinellid sponges, lithistid demosponges, non-rigid demosponges, Radiomura, Serpula (Dorsoserpula), Terebella, encrusting bryozoa, and minor contributions by calcareous sponges, and excavating sponges (type Aka). Thrombolites are dendrolitic and may reach sizes of several tens of centimeters, similar to the maximum size of siliceous sponges. The upper mound interval appears retrogradational and geometries change upsection from mound shapes to Bat lenses and level-bottom, biostromal sponge banks. The biotic assemblage is similar to that of the middle mound interval and there is no difference between mound and bank communities. The demise of sponge mounds is successive from regional spread in the Sinemurian to more localised spots in the Lower Pliensbachian. This reduction correlates with an increasing influence of pelagic conditions. At Foum Tillicht, sponge mounds lack any photic contribution and there is virtually no differentiation into subcommunities between mound surface and cavity dwelling organisms. There is some evidence that the heterotrophic food web of mound communities was sourced by oxygen minimum zone edge effects, namely microbial recycling of essential elements such as N and P. Basin geometry suggests a waterdepth of several 100's of meters, well below the photic zone and possibly only controlled by the depth range of the oxygen minimum zone. Palaeoceanographic conditions of well-stratified deeper water masses diminished gradually during widespread transgression across the Sinemurian to Pliensbachian boundary culminating in the Lower Pliensbachian ibex ammonite zone."],["dc.identifier.doi","10.1007/BF02668177"],["dc.identifier.isi","000169417700015"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/31770"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Institut Palaontologie Universitat Erlangen-nurnberg"],["dc.relation.issn","0172-9179"],["dc.title","Facies of Liassic sponge mounds, central High Atlas, Morocco"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","681"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","Geology"],["dc.bibliographiccitation.lastpage","684"],["dc.bibliographiccitation.volume","31"],["dc.contributor.author","Neuweiler, F."],["dc.contributor.author","d'Orazio, V."],["dc.contributor.author","Immenhauser, A."],["dc.contributor.author","Geipel, G."],["dc.contributor.author","Heise, K. H."],["dc.contributor.author","Cocozza, C."],["dc.contributor.author","Miano, T. M."],["dc.date.accessioned","2018-11-07T10:37:16Z"],["dc.date.available","2018-11-07T10:37:16Z"],["dc.date.issued","2003"],["dc.description.abstract","Intracrystalline organic compounds, enclosed within in situ-precipitated marine microcrystalline calcite (automicrite), might represent either an inclusion or the catalyst of such precipitation. We use evidence from a Lower Cretaceous deep-water carbonate mound to show (1) the original source, (2) the degree of condensation, (3) the redox conditions involved, and (4) the catalytic role of natural organic matter for the precipitation of automicrite. Fluorescence spectrometry of the intracrystalline organic fraction extracted from these carbonates identifies a marine fulvic acid-like organic compound with a low degree of pollycondensation. This finding points to a temporal correlation of the initial stage of geo-polymer formation with the precipitation of automicrite. Furthermore, the rare earth element (REE) distribution patterns in the mineral show a consistent positive Ce anomaly, suggesting an episode of reductive dissolution of iron-manganese oxyhydroxides during automicrite formation. In general, a relative enrichment of middle-weight REEs is observed, resulting in a convex distribution pattern typical for, e.g., phosphate concretions or humic acid material. By merging the results of spectrometry and REE geochemistry we thus conclude that the marine calcite precipitation was catalyzed by marine fulvic acid-like compounds during the early stages of humification under suboxic conditions. This indicates that humification, driven by the presence of a benthic biomass, is more important for calcite authigenesis than any site-specific microbial metabolism. The Neoproterozoic rise of carbonate mounds supports this hypothesis; there is molecular evidence for early metazoan divergence then, but not for a major evolutionary episode of microorganisms."],["dc.identifier.doi","10.1130/G19775.1"],["dc.identifier.isi","000184658400007"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/45521"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Geological Soc Amer, Inc"],["dc.relation.issn","1943-2682"],["dc.relation.issn","0091-7613"],["dc.title","Fulvic acid-like organic compounds control nucleation of marine calcite under suboxic conditions"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","195"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Facies"],["dc.bibliographiccitation.lastpage","284"],["dc.bibliographiccitation.volume","36"],["dc.contributor.author","Neuweiler, Fritz"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Monty, Claude"],["dc.contributor.author","Feldmann, Mark"],["dc.contributor.author","Awramik, Stan"],["dc.contributor.author","Bourque, Pierre-André"],["dc.contributor.author","Cirilli, Simonetta"],["dc.contributor.author","Gautret, Pascale"],["dc.contributor.author","Marcoux, Jean"],["dc.contributor.author","Plaziat, Jean Claude"],["dc.contributor.author","Defarge, Christian"],["dc.contributor.author","Trichet, Jean"],["dc.contributor.author","Pinckney, James L."],["dc.contributor.author","Bertrand-Sarfati, Janine"],["dc.contributor.author","Moussine-Pouchkine, Alexis"],["dc.contributor.author","Reid, Pamela"],["dc.contributor.author","Merz-Preiß, Martina"],["dc.contributor.author","Labiaux, Sébastien"],["dc.contributor.author","Baud, Aymon"],["dc.contributor.author","Thiel, Volker"],["dc.contributor.author","Michaelis, Walter"],["dc.contributor.author","Galling, Ursula"],["dc.contributor.author","Mäcker, Hartmut"],["dc.contributor.author","Arp, Gernot"],["dc.contributor.author","Krutschinna, Jenny"],["dc.contributor.author","Riding, Robert"],["dc.contributor.author","Webb, Greogory E."],["dc.contributor.author","Jell, John S."],["dc.contributor.author","Freiwald, André"],["dc.contributor.author","Mohanti, Manmohan"],["dc.contributor.author","Srikanta, S. S."],["dc.contributor.author","Bergbauer, Matthias"],["dc.contributor.author","Schumann-Kindel, Gabriela"],["dc.contributor.author","Manz, Werner"],["dc.contributor.author","Szewzyk, Ulrich"],["dc.date.accessioned","2019-11-06T10:55:04Z"],["dc.date.available","2019-11-06T10:55:04Z"],["dc.date.issued","1997"],["dc.identifier.doi","10.1007/BF02536885"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62575"],["dc.language.iso","en"],["dc.relation.issn","0172-9179"],["dc.relation.issn","1612-4820"],["dc.title","Biosedimentology of Microbial Buildups IGCP Project No. 380 Proceedings of 2nd Meeting, Göttingen/Germany 1996"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]