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Carbonate factories: A conundrum in sedimentary geology

Describing, characterizing and interpreting the nearly infinite variety of carbonate rocks are conundrums intricate and difficult problems having only The carbonate factories model, as defined at the beginning of the century, provides a subdivision of marine carbonate sediment production-systems based on the Marine carbonate factories: Review and update Reijmer 2021

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Understanding carbonate factories through palaeoecological and

proposed a re-evaluation of Schlager’s concept of carbonate factory. According to these authors, a carbonate factory is identified as a carbonate Ecological niche modelling coupled with deep-time general circulation models is used to calibrate a predictive tool of carbonate factory distribution. A Marine carbonate factories: a global model of carbonate

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Global distribution of modern shallow-water marine

Abstract. Prediction of carbonate distributions at a global scale through geological time represents a challenging scientific issue, which is critical for carbonate reservoir studies and theThe extinction of most heavy calcifiers, such as corals, calcareous algae and sponges, during the Permian-Triassic mass extinction (PTME) coincides with the Carbonate factories: A conundrum in sedimentary geology

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Carbonate factories and their critical control on the geometry of

Abstract. Tropical rimmed platforms represent a much more efficient protection from coastal erosion than carbonate ramps. Understanding the controlling A carbonate factory is a carbonate precipitation mode defined by an ecosystem (cf. James and Jones, 2015; Michel et al., 2019). Definitions of factories come Stratigraphic evolution and carbonate factory

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Controls on large-scale architecture and facies ScienceDirect

Carbonate factories (or carbonate production systems) are primarily controlled by water chemistry and oceanographic setting and exert an impact on the Platform morphologies and slope profiles are also factory specific: T-factories show a rimmed flat-topped platform with adjacent exponential slopes or a carbonate ramp morphology; CWC-factories display mound morphologies with steep slopes; C-factories are associated with open shelf systems and Gaussian shaped slope Marine carbonate factories: Review and update Reijmer 2021

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The evolution of the marine carbonate factory Semantic Scholar

Calcium carbonate formation is the primary pathway by which carbon is returned from the ocean–atmosphere system to the solid Earth^ 1,2 . The removal of dissolved inorganic carbon from seawater by precipitation of carbonate minerals—the marine carbonate factory—plays a critical role in shaping marine biogeochemical According to this relationship, six basic geometric patterns of the carbonate platforms were summarized, namely progradation with aggradation, aggradation, back-stepping, "empty bucket," drowningSedimentology and sequence stratigraphy of carbonate rocks

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The "Carbonate Factory" Revisited: A Reexamination of Sediment

There are two widely used models of sediment production on carbonate shelves: (1) production varying with depth, and (2) production as a function of depth and distance from the platform margin. Here we recalculate carbonate production on Great Bahama Bank west and northwest of Andros Island using Broecker and Takahashi's (1966) pioneering Noel James, Professor of Geology at Queen’s University, Canada, has, for over 40 years focused his research on carbonate sediments and rocks that range from the modern seafloor to the Archean, studying their origin via extensive marine and terrestrial fieldwork, petrography, and geochemistry. He has taught numerous courses on oceanography, Origin of Carbonate Sedimentary Rocks Wiley

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A subseafloor carbonate factory across the Triassic-Jurassic

Abstract. Triassic-Jurassic (T-J) boundary successions record a paucity of carbonate in association with the mass extinction. Here we demonstrate that three globally disparate T-J sections contain volumetrically important early diagenetic carbonate, i.e., carbonate formed soon after deposition of the sediment but commonly ignored as Read (1982Read (,1985 differentiated carbonate ramps as either homoclinal, characterised by uniform gentle dips, usually less than 1°(e.g., Elrick and Read, 1991;Burchette and Wright, 1992Carbonate systems Request PDF ResearchGate

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Stratigraphic evolution and carbonate factory implications: Case study

By observing modern carbonate systems, at a carbonate platform scale, Schlager (2000; 2003; 2005) defined and individualized three different marine precipitation modes based on stratigraphic and diagenetic principles, that is T/tropical, C/cool water and M/microbial or mud-mound factories, each factory with its own characteristics regarding Then, spatial analysis is used to calibrate different carbonate factory functions that predict oceanic zones favorable to specific carbonate factories. Geology 32, 213–216 (2004).Global distribution of modern shallow-water marine carbonate factories

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The mantle, CO2 and the giant Aptian chemogenic lacustrine carbonate

During the Aptian (Cretaceous), in what is now the South Atlantic, the largest chemogenic (abiotic) carbonate factory so far identified in the Phanerozoic geological record developed as a vast hyper‐alkaline lake system. This covered at least 330 000 km2, producing carbonates, locally over 500 m thick, in what are now the offshore Stratigraphic evolution and carbonate factory implications: Case study of the Albian carbonates of the Campos Basin, Brazil June 2020 The Depositional Record 7(3)(PDF) Stratigraphic evolution and carbonate factory

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Carbonate factory turnovers influenced by the monsoon (Xisha

Carbonate factory turnovers are the integrated result of climatic, oceanographic and biological controls. Sedimentological, geochemical and palaeontological data from core XK-1 drilled in the Xisha Islands, South China Sea, reveal that photozoan to heterozoan carbonate factory turnovers during the Early and Middle Miocene in isolated Because organic carbon contains a larger fraction of the light isotope 12 C than inorganic carbonate, variations in the carbon isotopic record of sedimentary rocks are thought to represent changes in the Authigenic Carbonate and the History of the Global

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Seeking a geochemical identifier for authigenic carbonate

Figure 1: Geochemical results of sedimentary carbonates from the Yindushan section. ( a) A δ 13 C carb –δ 18 O carb cross-plot for all samples. ( b) Stratigraphic variations of δ 13 C carbHamelin Pool, located in Shark Bay, Western Australia, (Fig. 1 a), is a restricted embayment about 800 km north of Perth, Western Australia. Hamelin Pool covers roughly 1400 square kilometers andThe microbial carbonate factory of Hamelin Pool, Shark Bay,

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Facies and evolution of the carbonate factory during the Permian

The nature of Phanerozoic carbonate factories is strongly controlled by the composition of carbonate-producing faunas. During the Permian–Triassic mass extinction interval there was a major change in tropical shallow platform facies: Upper Permian bioclastic limestones are characterized by benthic communities with significant Chaper 7 introduced carbonate sequence stratigraphy with a detailed look at the T factory the best known carbonate system and the most productive one. The present chapter deals with the sequence stratigraphy of the C and M factories. It does so by high-lighting differences to the T factory.Carbonate Sedimentology and Sequence Stratigraphy

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Carbonates SEPM Strata

This page leads into portions of a course on Carbonate Petrology. It provides access to photomicrographs and a series of exercises related to over 240 different thin sections of carbonate Rock s. Some 1,700 images were captured, and as a result some thin sections have over ten images associated with them. The intent of this site is to provide1. Introduction. Carbonate factories are characterized by specific depth ranges where carbonate sediment is generated from either biotic or abiotic processes and varies in composition and production rates (Reijmer, 2021).Carbonate factories (or carbonate production systems) are primarily controlled by water chemistry and Controls on large-scale architecture and facies ScienceDirect

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carbonate factory géologie vidéo

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