Academic literature on the topic 'Stromatolithes'

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Journal articles on the topic "Stromatolithes"

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Legrand, Philippe, Pierre Debriette, Stephen Durif, and Ronny Roessler. "Flore autunienne silicifiée de Gipcy (permien inferieur du bassin de Bourbon-l’Archambault, Allier, Massif Central, France)." Annales de la Société géologique du Nord - (2e Série), Tome XXX, no. 30 (December 15, 2023): 79–90. http://dx.doi.org/10.54563/asgn.2288.

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La flore autunienne de Gipcy (Permien inférieur du bassin de Bourbon-l'Archambault) est pour la première fois décrite et figurée. Cette flore bien conservée comprend essentiellement des stromatolithes silicifiés, des tiges perminéralisées de Calamites Suckow identifiées comme Arthropitys Goeppert, des racines de Psaronius Cotta, et des morceaux de bois pycnoxyliques silicifiés Agathoxylon Hartig. Parmi les Agathoxylon, des tiges à structure conservée ont été rapprochées des Cordaites et des Conifères.Des valves d'ostracodes ont aussi été observées au voisinage des laminations stromatolithiques
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Brook, George A., A. Cherkinsky, L. Bruce Railsback, Eugene Marais, and Martin H. T. Hipondoka. "14C Dating of Organic Residue and Carbonate from Stromatolites in Etosha Pan, Namibia: 14C Reservoir Effect, Correction of Published Ages, and Evidence of >8-m-Deep Lake During the Late Pleistocene." Radiocarbon 55, no. 3 (2013): 1156–63. http://dx.doi.org/10.1017/s0033822200048062.

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Lacustrine stromatolites are layered accretionary structures formed in shallow water by cyanobacteria. They are a precise indicator of high lake limits and their morphology and structure provide an insight into paleoenvironments of the time. Previous research on lacustrine stromatolites from Etosha Pan in Namibia based on radiocarbon ages of carbonates were close to the limit of the method and did not account for any possible 14C reservoir effect. The ages were used to suggest that the basin was not extensively flooded during the last 40,000 yr. To assess the reservoir effect, the age characte
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Rakhmanova, А. V. "History of the study of Karelia Paleoproterozoic stromatolites and their display at the Museum of Precambrian Geology, Petrozavodsk." Vestnik of Geosciences 4 (2021): 25–31. http://dx.doi.org/10.19110/geov.2021.4.4.

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The paper deals with the history of stromatolite studies in the Republic of Karelia and the compiling of a stromatolite collection at the Museum of Precambrian Geology, IG, KarRC, RAS, Petrozavodsk. Major stages in the study of Karelia’s Proterozoic stromatolites are presented, changes in the point of view of their origin are assessed and the exposition «Karelia’s and worldwide stromatolites» is described for the first time. Analysis of the history of Karelia’s widespread and accessible stromatolites and a review of the stromatolite collection at the museum are of scientific and educational in
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Papineau, Dominic, Jeffrey J. Walker, Stephen J. Mojzsis, and Norman R. Pace. "Composition and Structure of Microbial Communities from Stromatolites of Hamelin Pool in Shark Bay, Western Australia." Applied and Environmental Microbiology 71, no. 8 (2005): 4822–32. http://dx.doi.org/10.1128/aem.71.8.4822-4832.2005.

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ABSTRACT Stromatolites, organosedimentary structures formed by microbial activity, are found throughout the geological record and are important markers of biological history. More conspicuous in the past, stromatolites occur today in a few shallow marine environments, including Hamelin Pool in Shark Bay, Western Australia. Hamelin Pool stromatolites often have been considered contemporary analogs to ancient stromatolites, yet little is known about the microbial communities that build them. We used DNA-based molecular phylogenetic methods that do not require cultivation to study the microbial d
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Antropova, E. "A new location of stromatolites in the Middle Timan: their morphological and structural features." Vestnik of geosciences, no. 12 (February 21, 2024): 24–29. http://dx.doi.org/10.19110/geov.2023.12.3.

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The paper presents the results of macroscopic and microscopic study of Riphean stromatolites of the Pavyuga Formation from a new locality on the left bank of the Vorykva River (Middle Timan). The stromatolites form a stromatolite bioherm. The microstructure of the stromatolite assemblages is characterised by layering of different composition and granularity; traces of organogenic formations of clotted and filamentous type were found in microgranular interlayers. Numerous traces of secondary transformations, such as pyritization, dolomitization on shells, and fenestra formation, were noted. The
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Villafañe, Patricio Guillermo, Carlos Cónsole-Gonella, Paolo Citton, Ignacio Díaz-Martínez, and Silvina de Valais. "Three-dimensional stromatolites from Maastrichtian–Danian Yacoraite Formation, Argentina: modelling and assessing hydrodynamic controls on growth patterns." Geological Magazine 158, no. 10 (2021): 1756–72. http://dx.doi.org/10.1017/s0016756821000315.

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AbstractStromatolites are biogenic sedimentary structures formed by the interplay of biological (microbial composition) and environmental factors (local hydrodynamic conditions, clastic input and/or water chemistry). Well-preserved, three-dimensional (3D) fossil stromatolites are key to assessing the environmental factors controlling their growth and resulting morphology in space and time. Here, we report the detailed analysis of well-exposed, highly informative stromatolite build-ups from a single stratigraphic horizon within the Maastrichtian–Danian Yacoraite Formation (Argentina). This stud
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Douglas, Susanne, Meredith E. Perry, William J. Abbey, Zuki Tanaka, Bin Chen, and Christopher P. McKay. "The structure and chemical layering of Proterozoic stromatolites in the Mojave Desert." International Journal of Astrobiology 14, no. 3 (2015): 517–26. http://dx.doi.org/10.1017/s1473550415000026.

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AbstractThe Proterozoic carbonate stromatolites of the Pahrump Group from the Crystal Spring formation exhibit interesting layering patterns. In continuous vertical formations, there are sections of chevron-shaped stromatolites alternating with sections of simple horizontal layering. This apparent cycle of stromatolite formation and lack of formation repeats several times over a vertical distance of at least 30 m at the locality investigated. Small representative samples from each layer were taken and analysed using X-ray diffraction (XRD), X-ray fluorescence (XRF), environmental scanning elec
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Riding, Robert. "Abiogenic, microbial and hybrid authigenic crusts: components of Precambrian stromatolites." Geologia Croatica 61, no. 2-3 (2008): 73–103. http://dx.doi.org/10.4154/gc.2008.10.

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Authigenic seafloor carbonate crusts include fenestrate microbialite, thrombolite, and four types here designated Fine-grained Crust, Sparry Crust, Hybrid Sparry Fine-grained Crust, and Sparry Crust plus Coarse Grains. Each of the latter four types includes at least some layered examples that have generally been regarded as stromatolites. Recognition and interpretation of these various deposits assists understanding of stromatolite development. Sparry Crust is common in the Late Archaean-Mesoproterozoic. It includes botryoidal fans and other crystal pseudomorphs, microdigitate stromatolite, de
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Keim, Carolina N., Hélisson Nascimento dos Santos, Carolina Souza Santiago, et al. "Microstructure and mineral composition of Holocene stromatolites from Lagoa Vermelha, a hypersaline lagoon in Brazil: Insights into laminae genesis." Journal of Sedimentary Research 90, no. 8 (2020): 887–905. http://dx.doi.org/10.2110/jsr.2020.40.

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ABSTRACT Stromatolites are domes, columns, or nearly flat crusts of laminated sedimentary rocks, usually consisting of Ca-Mg carbonates. Stromatolites result from lithification of microbial mats, which are benthic microbial ecosystems where microorganisms arrange themselves in layers according to their physiology. Despite a century of research, the hypothesis of stromatolite genesis by lithification of microbial mats remains controversial, and a convincing explanation for how stromatolites arise from microbial mats is still lacking. In this work, we analyze in detail a stromatolite from Lagoa
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Hofmann, H. J., and A. Davidson. "Paleoproterozoic stromatolites, Hurwitz Group, Quartzite Lake area, Northwest Territories, Canada." Canadian Journal of Earth Sciences 35, no. 3 (1998): 280–89. http://dx.doi.org/10.1139/e97-103.

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Decimetric to metric domal stromatolites with constituent ministromatolites characterize reddish, 13C-enriched dolostones in the Watterson Formation of the Quartzite Lake area west of Hudson Bay. They provide paleontologic support for a correlation with the only other known early Paleoproterozoic stromatolite occurrences in North America: the Kona Formation of Michigan, and the Nash Formation in southern Wyoming. They also are similar to stromatolites in probable coeval Jatulian carbonates in Karelia on the Baltic Shield, and possibly to stromatolites in the Hutuo Group in China.
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Dissertations / Theses on the topic "Stromatolithes"

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Garnier-Caudwell, Christiane. "Eude expérimentale de la croissance de stromatolithes a rivularia actuels et subactuels, d'eau douce, en climat tempéré." Dijon, 1995. http://www.theses.fr/1995DIJOS043.

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Des stromatolithes a rivularia haematites (d. C. ) Agardh et a rivularia biasolettiana meneghini, prélevés sur le plateau de Langres (France) en milieu palustre, ont été suivis sur le terrain, transplantes en milieu fluviatile et cultives sur des milieux favorables dans des conditions de température et d'éclairement variables suivant des cycles jour-nuit. Chez rivularia haematites, la formation d'une bande sombre micritique se fait en trois étapes. La première correspond à l'édification uniquement biologique de zones sombres, ou niveaux à gaines, grâce à l'alignement des heterocystes et des fa
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De, Wever Alexis. "Étude de la biominéralisation de carbonates intracellulaires et de silicates de magnésium hydratés dans des environnements lacustres alcalins." Electronic Thesis or Diss., Sorbonne université, 2019. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2019SORUS480.pdf.

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Les stromatolites sont des roches organo-sédimentaires laminées composées de carbonates de Ca et/ou Mg mais également de silicates de Mg dans certains cas. Les processus impliqués dans leur formation restent encore mal compris. L’objectif central de cette thèse est de mieux comprendre les processus géochimiques et géomicrobiologiques permettant de favoriser ou au contraire de défavoriser la formation des carbonates et silicates de magnésium dans les environnements lacustres alcalins mexicains. Deux axes principaux ont été développés. Le premier axe s’est focalisé sur les analyses de souches fo
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Debrie, Juliette. "Traçage des conditions environnementales et de l'activité microbienne dans des stromatolites formés en contexte évaporitique : stromatolites actuels de Sardaigne et stromatolites du Messinien (6Ma)." Electronic Thesis or Diss., Sorbonne université, 2022. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2022SORUS454.pdf.

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Les stromatolites sont des structures organo-sédimentaires laminées, formées grâce à l’activité microbienne. Présents depuis plus de 3,5 milliards d’années, ils comptent parmi les plus anciennes traces de vie connues sur Terre et ils fournissent des informations précieuses sur la paléobiodiversité et les paléoenvironnements. De nombreuses études ont permis de développer une connaissance approfondie sur les stromatolites actuels, marins et lacustres, pouvant servir de référence pour l’interprétation des stromatolites anciens. Cependant, peu de travaux concernent des stromatolites d'environnemen
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Miningou, Mariette. "Genèse des indices polymétallifères des formations néoprotérozoïques (1000 – 543 Ma) dans la région du Béli (Nord du Burkina Faso) : contrôle structural, nature des fluides, rôle de la silice." Aix-Marseille 3, 2006. http://www.theses.fr/2006AIX30068.

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A l’instar des formations sédimentaires des bassins de Taoudeni et des Volta, celles de la région du Béli comportent une triade (tillite-calcaire-silexite) et une formation molassique. Ces marqueurs stratigraphiques ont permis la subdivision verticale des ensembles sédimentaires des bassins ouest-africains en trois surpergroupes. La triade repose sur des grès-quartzites et est surmontée par des shales et des dolomies. Comme les formations carbonatées, certaines roches du complexe silexitique renferment des stromatolites, de même que des micro-organismes. Dans la région du Béli, excepté le deux
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Feldmann, Markus. "Controls on stromatolite formation : a comparative study of modern stromatolites from the Bahamas with Messinian examples from Southeast Spain /." [S.l.] : [s.n.], 1995. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=11119.

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Garcin, Manuel. "Le bassin de San Miguel de Salinas (Alicante, Espagne) : relations entre contexte structuro-sédimentaire et dépôts évaporitiques et carbonates au Messinien." Paris 11, 1987. http://www.theses.fr/1987PA112027.

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Cette étude traite de l'évolution d'un bassin messinien, a termes évaporitiques du Levant espagnol ainsi que de son histoire pliocène et quaternaire. Dans un premier temps, l'analyse des dépôts, sous les aspects lithologique, sédimentologique et micropaléontologique est effectuée; des évaluations bathymétriques et paléoenvironnementales en sont dégagées. Les rapports géométriques des différents corps sédimentaires et notamment ceux des carbonates et des évaporites du Messinien, sont déduits de la carte au I:25000 et des observations de terrains. Différents processus sédimentaires aussi bien ch
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Couradeau, Estelle. "Géomicrobiologie des microbialites du lac alcalin d'Alchichica (Mexique)." Phd thesis, Université Paris-Diderot - Paris VII, 2012. http://tel.archives-ouvertes.fr/tel-00934407.

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Les stromatolites sont des structures organo-sédimentaires formées grâce à l'activité des microorganismes. Ils dominent le registre fossile Précambrien et sont parmi les plus anciennes traces potentielles de vie sur Terre (datées à 3,5 Ga). Cependant les processus biotiques et abiotiques à l'origine de leur formation restent peu compris et ouvrent des débats sur leur interprétation. L'objectif central de ce travail est de contribuer à améliorer notre compréhension de la formation des microbialites modernes, en particulier du rôle et du devenir des microorganismes dans ces systèmes afin de mieu
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Couradeau, Estelle. "Géomicrobiologie des microbialites du lac Alcalin d'Alchichica (Mexique)." Phd thesis, Paris 7, 2012. http://www.theses.fr/2012PA077015.

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Les stromatolites sont des structures organo-sédimentaires formées grâce à l'activité des microorganismes. Ils dominent le registre fossile Précambrien et sont parmi les plus anciennes traces potentielles de vie sur Terre, Cependant les processus biotiques et abiotiques à l'origine de leur formation restent peu compris. L'objectif central de ce travail est de contribuer à améliorer notre compréhension de la formation des microbialites modernes, afin de mieux contraindre l'interprétation du registre fossile des stromatolites. Nous avons étudié le système modèle des microbialites modernes du lac
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Petroff, Alexander Peter Phillips. "Streams, stromatolites and the geometry of growth." Thesis, Massachusetts Institute of Technology, 2011. http://hdl.handle.net/1721.1/68996.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2011.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (p. 148-159).<br>This collection of papers is about recognizing common geometric features in the dynamics shaping diverse phenomena in the natural world. In particular, we focus on two systems which grow in response to a diffusive flux. The first system is a microbial mat which overlays a layer of precipitated mineral. The microbial mat grows in response to the diffusion of nutrients while the mineral
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Davis, Burton S. "Stromatolites in the upper lacustrine unit of the Paleocene Hanna Formation, Hanna Basin, south-central Wyoming." Laramie, Wyo. : University of Wyoming, 2006. http://proquest.umi.com/pqdweb?did=1136088711&sid=2&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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Books on the topic "Stromatolithes"

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Stromatolites. Western Australian Museum, 1992.

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Reitner, Joachim, Nadia-Valérie Quéric, and Mike Reich, eds. Geobiology of Stromatolites. Göttingen University Press, 2008. http://dx.doi.org/10.17875/gup2008-235.

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Bertrand-Sarfati, Janine, and Claude Monty, eds. Phanerozoic Stromatolites II. Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-1124-9.

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Janine, Bertrand-Sarfati, and Monty Claude 1937-, eds. Phanerozoic stromatolites II. Kluwer Academic Publishers, 1994.

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Riding, Robert, ed. Calcareous Algae and Stromatolites. Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/978-3-642-52335-9.

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1937-, Valdiya K. S., Tewari V. C, Wadia Institute of Himalayan Geology., and Indo-Soviet Symposium on "Stromatolites and Stromatolitic Deposits" (1988 : Dehra Dun, India), eds. Stromatolites and stromatolitic deposits. Wadia Institut of Himalayan Geology, 1989.

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Robert, Riding, and International Symposium on Fossil Algae (4th : 1987 : Cardiff, Wales), eds. Calcareous algae and stromatolites. Springer-Verlag, 1991.

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Reitner, Joachim, Nadia-Valérie Quéric, and Gernot Arp. Advances in Stromatolite Geobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-10415-2.

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(Joachim), Reitner J., Quéric Nadia-Valérie, Arp Gernot 1968-, Deutsche Forschungsgemeinschaft, and Universität Göttingen, eds. Advances in stromatolite geobiology. Springer, 2010.

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Joseph, Seckbach, and SpringerLink (Online service), eds. STROMATOLITES: Interaction of Microbes with Sediments. Springer Science+Business Media B.V., 2011.

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Book chapters on the topic "Stromatolithes"

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McLoughlin, Nicola. "Stromatolites." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_1528.

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Sokolov, Boris S., and Andrew B. Iwanowski. "Stromatolites." In The Vendian System. Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-73972-9_10.

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McLoughlin, Nicola. "Stromatolites." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_1528.

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Reid, R. Pamela. "Stromatolites." In Encyclopedia of Modern Coral Reefs. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2639-2_152.

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McLoughlin, Nicola. "Stromatolites." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-642-27833-4_1528-4.

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McLoughlin, Nicola. "Stromatolites." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_1528-3.

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McLoughlin, Nicola. "Stromatolites." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_1528.

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Gooch, Jan W. "Stromatolite." In Encyclopedic Dictionary of Polymers. Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-6247-8_14876.

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Moore, L. S., and R. V. Burne. "The Modern Thrombolites of Lake Clifton, Western Australia." In Phanerozoic Stromatolites II. Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-1124-9_1.

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Soudry, D., and G. Panczer. "Stromatolic Phosphorites in the Eocene of the Negev (Southern Israel)." In Phanerozoic Stromatolites II. Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-1124-9_10.

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Conference papers on the topic "Stromatolithes"

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Dyakova, S. A., T. V. Litvinova, and N. D. Sergeeva. "BIOGENIC ULTRAMICROSTRUCTURES IN RIPHEAN STROMATOLITES IN THE VOLGA-URALIAN AREA (EAST RUSSIAN PLATE)." In Проблемы минералогии, петрографии и металлогении. Научные чтения памяти П. Н. Чирвинского. Perm State University, 2023. http://dx.doi.org/10.17072/chirvinsky.2023.35.

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The article presents the results of a study of core samples, including stromatolite dolomites of the Kaltasa (Lower Riphean) and Leuza (Upper Riphean) formations of the Volga-Uralian area of Russia. Using a scanning electron microscope, fossilized remains of coccoid and filamentous microfossils, as well as fragments of bacterial biofilms accompanying them, were found in stromatolites. The nature of biogenic ultramicrostructures is confirmed by the determination of the elemental composition. Fossilized relics of organisms are characterized by the presence of biophilic elements and increased car
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Storrie-Lombardi, Michael C., and Stanley M. Awramik. "A sideways view of stromatolites: complexity metrics for stromatolite laminae." In SPIE Optics + Photonics, edited by Richard B. Hoover, Gilbert V. Levin, and Alexei Y. Rozanov. SPIE, 2006. http://dx.doi.org/10.1117/12.679869.

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Mahseredjian, Taleen, Dylan T. Wilmeth, Frank A. Corsetti, Olivia Piazza, and Carie M. Frantz. "INTRA-LAMINATION ISOTOPIC VARIABILITY IN GREEN RIVER FORMATION STROMATOLITES: SIGNIFICANCE FOR STROMATOLITE-BASED PALEOCLIMATE MODELING OF THE EARLY EOCENE CLIMATIC OPTIMUM." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300883.

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Ulmer-Scholle, Dana S. "Stromatolites in the Todilto Formation?" In 56th Annual Fall Field Conference. New Mexico Geological Society, 2005. http://dx.doi.org/10.56577/ffc-56.380.

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Awramik, Stanley M., and Kathleen Grey. "Stromatolites: biogenicity, biosignatures, and bioconfusion." In Optics & Photonics 2005, edited by Richard B. Hoover, Gilbert V. Levin, Alexei Y. Rozanov, and G. Randall Gladstone. SPIE, 2005. http://dx.doi.org/10.1117/12.625556.

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C. Kuroda, M., A. M. Carvalho, and A. C. Vidal. "Classification of Stromatolites Using SOM." In 73rd EAGE Conference and Exhibition incorporating SPE EUROPEC 2011. EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20149712.

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"Microbial structure in the Visean deposits of the Ilych river (Northern Urals)." In All-Russia Lithological Meeting «Geology of reefs». Institute of Geology FRC Komi SC UB RAS, 2020. http://dx.doi.org/10.19110/98491-013-134-136.

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The paper presents data on the distribution of microbial formations in the Visean rocks of the Ilych River basin (Northern Urals). They were found to be present in significant numbers only in the Venevian level. Stromatolites were found in the Visean on the Ilych River for the first time.
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Corsetti, Frank, Carie M. Frantz, Victoria A. Petryshyn, Yadira Ibarra, and Dylan Wilmeth. "STROMATOLITE BIOGENICITY: AN UPDATE." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-368005.

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Proctor, Jacob, Pedro H. Vieira de Luca, Gustavo Antunes Pimentel, et al. "Porosity and Permeability upscaling in a Lagoa Salgada Stromatolite and Codó Formation Stromatolite." In 14th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 3-6 August 2015. Brazilian Geophysical Society, 2015. http://dx.doi.org/10.1190/sbgf2015-154.

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Bruihler, Sarah, Lindsey Reiners, Tanner Eischen, and Julie K. Bartley. "RELATIONSHIPS BETWEEN MICROSTRUCTURE AND MORPHOLOGY IN LACUSTRINE STROMATOLITES." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-304048.

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Reports on the topic "Stromatolithes"

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Joseph, Rhawn. Mars: Algae, Lichens, Fossils, Minerals, Microbial Mats, and Stromatolites in Gale Crater. Journal of Astrobiology and Space Science, 2020. http://dx.doi.org/10.37720/jassr.03082020.

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