Reitner, Joachim

[["dc.bibliographiccitation.firstpage","473"],["dc.bibliographiccitation.lastpage","506"],["dc.contributor.author","Bouougri, El Hafid"],["dc.contributor.author","Porada, Hubertus"],["dc.contributor.author","Weber, Klaus"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.editor","Reitner, Joachim"],["dc.contributor.editor","Quéric, Nadia Valérie"],["dc.contributor.editor","Arp, Gernot"],["dc.date.accessioned","2019-11-06T10:19:53Z"],["dc.date.available","2019-11-06T10:19:53Z"],["dc.date.issued","2011"],["dc.description.abstract","The Ediacaran was a period of wide soft-bodied biota development in marine siliciclastic environment. The reconstruction of palaeoecology, lifestyle and environment settings of these organisms are among the challenges in characterising the earliest metazoan life on Earth. The biota colonised sea bottoms and were living as benthic communities occurring in a wide spectrum of environmental settings (e.g. Gehling 2000; Waggoner 2003; Narbonne 2005; Grazhdankin 2004; Droser et al. 2006). In the classical localities (e.g. Newfoundland, Namibia, White Sea and Australia), the fossils occur in rock successions with distinct depositional settings ranging from distributary mouth-bar of braid-delta systems to deep-water slope (Gehling 2000; Grazhdankin 2004; Narbonne 2005)."],["dc.identifier.doi","10.1007/978-3-642-10415-2_29"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62574"],["dc.language.iso","en"],["dc.publisher","Springer"],["dc.publisher.place","Berlin"],["dc.relation.doi","10.1007/978-3-642-10415-2"],["dc.relation.isbn","978-3-642-10414-5"],["dc.relation.isbn","978-3-642-10415-2"],["dc.relation.ispartof","Advances in Stromatolite Geobiology"],["dc.relation.ispartofseries","Lecture Notes in Earth Sciences;131"],["dc.title","Sedimentology and Palaeoecology of Ernietta-Bearing Ediacaran Deposits in Southern Namibia: Implications for Infaunal Vendobiont Communities"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","221"],["dc.bibliographiccitation.lastpage","231"],["dc.bibliographiccitation.seriesnr","131"],["dc.contributor.author","Kurz, Jens"],["dc.contributor.author","Simon, Klaus"],["dc.contributor.author","Heim, Christine N."],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Quéric, Nadia Valérie"],["dc.contributor.author","Thiel, Volker"],["dc.contributor.editor","Reitner, Joachim"],["dc.contributor.editor","Quéric, Nadia Valérie"],["dc.contributor.editor","Arp, Gernot"],["dc.date.accessioned","2019-11-06T10:08:00Z"],["dc.date.available","2019-11-06T10:08:00Z"],["dc.date.issued","2011"],["dc.description.abstract","The Äspö Hard Rock Laboratory (Äspö HRL) is a tunnel located near Oskarshamn in the southeast of Sweden, that serves as a testing environment for the disposal of nuclear waste. The Äspö HRL hosts and makes accessible a wide spectrum of microbially driven subsurface ecosystems (Pedersen 1997)."],["dc.identifier.doi","10.1007/978-3-642-10415-2_15"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62569"],["dc.language.iso","en"],["dc.publisher","Springer"],["dc.publisher.place","Berlin"],["dc.relation.crisseries","Lecture Notes in Earth Sciences"],["dc.relation.doi","10.1007/978-3-642-10415-2"],["dc.relation.isbn","978-3-642-10414-5"],["dc.relation.isbn","978-3-642-10415-2"],["dc.relation.ispartof","Advances in Stromatolite Geobiology"],["dc.relation.ispartofseries","Lecture Notes in Earth Sciences;131"],["dc.relation.issn","0930-0317"],["dc.title","Trace Element and Biomarker Signatures in Iron-Precipitating Microbial Mats from the Tunnel of Äspö (Sweden)"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","265"],["dc.bibliographiccitation.lastpage","276"],["dc.bibliographiccitation.seriesnr","131"],["dc.contributor.author","Tribollet, Aline"],["dc.contributor.author","Golubic, Stjepko"],["dc.contributor.author","Radtke, Gudrun"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.editor","Reitner, Joachim"],["dc.contributor.editor","Quéric, Nadia Valérie"],["dc.contributor.editor","Arp, Gernot"],["dc.date.accessioned","2019-11-06T10:10:41Z"],["dc.date.available","2019-11-06T10:10:41Z"],["dc.date.issued","2011"],["dc.description.abstract","Destruction of rocks and minerals by biological activities has been termed bioerosion (Neumann 1966). It includes mechanical as well as chemical effects, i.e. bioabrasion and biocorrosion (Schneider 1976; Golubic and Schneider 1979). However both processes often co-occur; they are functionally interconnected and mutually supportive. Biocorrosion can result from the activity of macro- or micro- organisms and thus is called macrobiocorrosion and microbiocorrosion. Microbiocorrosion can also be closely associated with microbial rock formation and consolidation in stromatolitic structures (Reid et al. 2000; Macintyre et al."],["dc.identifier.doi","10.1007/978-3-642-10415-2_17"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62570"],["dc.language.iso","en"],["dc.relation.crisseries","Lecture Notes in Earth Sciences"],["dc.relation.doi","10.1007/978-3-642-10415-2"],["dc.relation.isbn","978-3-642-10414-5"],["dc.relation.isbn","978-3-642-10415-2"],["dc.relation.ispartof","Advances in Stromatolite Geobiology"],["dc.relation.ispartofseries","Lecture Notes in Earth Sciences;131"],["dc.relation.issn","0930-0317"],["dc.title","On Microbiocorrosion"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","409"],["dc.bibliographiccitation.lastpage","434"],["dc.bibliographiccitation.seriesnr","131"],["dc.contributor.author","Rodriguez-Martinez, Marta"],["dc.contributor.author","Heim, Christine N."],["dc.contributor.author","Simon, Klaus"],["dc.contributor.author","Zilla, Thomas"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.editor","Reitner, Joachim"],["dc.contributor.editor","Quéric, Nadia Valérie"],["dc.contributor.editor","Arp, Gernot"],["dc.date.accessioned","2019-11-06T10:15:52Z"],["dc.date.available","2019-11-06T10:15:52Z"],["dc.date.issued","2011"],["dc.description.abstract","Foraminifera are the most abundant sessile organisms found on ferromanganese crusts and nodules (Greenslate 1974; Wendt 1974; Dugolinsky et al. 1977; Riemann 1983; von Stackelberg 1984; Mullineaux 1987, 1988; Verlaan 1992; Resig and Glenn 1997; Toscano and Raspini 2005). In fact, actual ferromanganesecrusts and nodules share numerous similarities with their fossil counterparts."],["dc.identifier.doi","10.1007/978-3-642-10415-2_25"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62572"],["dc.language.iso","en"],["dc.publisher","Springer"],["dc.publisher.place","Berlin"],["dc.relation.crisseries","Lecture Notes in Earth Sciences"],["dc.relation.doi","10.1007/978-3-642-10415-2"],["dc.relation.isbn","978-3-642-10414-5"],["dc.relation.isbn","978-3-642-10415-2"],["dc.relation.ispartof","Advances in Stromatolite Geobiology"],["dc.relation.ispartofseries","Lecture Notes in Earth Sciences;131"],["dc.relation.issn","0930-0317"],["dc.title","Tolypammina gregaria Wendt 1969-Frutexites Assemblage and Ferromanganese Crusts: A Coupled Nutrient-Metal Interplay in the Carnian Sedimentary Condensed Record of Hallstatt Facies (Austria)"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","355"],["dc.bibliographiccitation.lastpage","390"],["dc.bibliographiccitation.seriesnr","131"],["dc.contributor.author","Delecat, Stefan"],["dc.contributor.author","Arp, Gernot"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.editor","Reitner, Joachim"],["dc.contributor.editor","Quéric, Nadia Valérie"],["dc.contributor.editor","Arp, Gernot"],["dc.date.accessioned","2019-11-06T10:13:39Z"],["dc.date.available","2019-11-06T10:13:39Z"],["dc.date.issued","2011"],["dc.description.abstract","In the aftermath of the Triassic–Jurassic extinction event, extant slopes of drowned alpine reef buildups were recolonized in patches by predominantly non-rigid sponges. Just a few localities in the Northern Calcareous Alps display autochthonous communities of these rarely in situ-preserved species and provide an insight into their taphonomy. In a depression of the former Triassic reef surface at Steinplatte (Austria) lyssacinosid sponges formed spicular mats during starved Liassic sedimentation. They settled on detrital soft- or firmgrounds that were successively dominated by spicules of their own death predecessors and infiltrated sediments. Skeletal remains and adjacent micrites were partly fixed by microbially induced carbonate precipitation due to the decay of sponge organic matter. The irregular compaction of the sediment as well as volume reduction during microbialite formation resulted in syndiagenetic stromatactis cavities. Subjacent to the spiculite allochthonous sediments fill up sinkholes and crevices of the rough Triassic relief. In order to define the Lower Liassic paleoenvironment, the sediments and associated ferromanganese crusts were analysed by X-ray fluorescence and ICP-mass spectrometry. The distribution pattern of major and trace elements show usual contents of hydrogeneous Fe/Mn-precipitates. In contrast, the results of rare earth element analyses revealed a negative Cerium anomaly within the crusts and the spiculite at Steinplatte locality. In Lower Liassic sediments of the Northern Calcareous Alps such an anomaly has been proved for the first time. Most likely it is related to higher precipitation rates caused by microbial mats or possibly by a minor influx of hydrothermal fluids. Carbon and oxygen stable isotopes of the same sequence show primary signals of a small negative δ13Ccarb excursion that extends from Hettangian to Lower Sinemurian time."],["dc.identifier.doi","10.1007/978-3-642-10415-2_23"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62571"],["dc.language.iso","en"],["dc.publisher","Springer"],["dc.publisher.place","Berlin"],["dc.relation.crisseries","Lecture Notes in Earth Sciences"],["dc.relation.doi","10.1007/978-3-642-10415-2"],["dc.relation.isbn","978-3-642-10414-5"],["dc.relation.isbn","978-3-642-10415-2"],["dc.relation.ispartof","Advances in Stromatolite Geobiology"],["dc.relation.ispartofseries","Lecture Notes in Earth Sciences;131"],["dc.relation.issn","0930-0317"],["dc.title","Aftermath of the Triassic–Jurassic Boundary Crisis: Spiculite Formation on Drowned Triassic Steinplatte Reef-Slope by Communities of Hexactinellid Sponges (Northern Calcareous Alps, Austria)"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]