A carbonate platform is a sedimentary body which possesses topographic relief, and is composed of autochthonous calcareous deposits (Wilson, 1975). Platform growth is mediated by sessile organisms whose skeletons build up the reef or by organisms (usually microbes) which induce carbonate precipitation through their metabolism. Therefore, carbonate platforms can not grow up everywhere: they are not present in places where limiting factors to the life of reef-building organisms exist. Such limiting factors are, among others: light, watertemperature, transparency and pH-Value. For example, carbonate sedimentation along the AtlanticSouth American coasts takes place everywhere but at the mouth of the Amazon River, because of the intense turbidity of the water there (Carannante et al., 1988). Spectacular examples of present-day carbonate platforms are the Bahama Banks under which the platform is roughly 8km thick, the Yucatan Peninsula which is up to 2km thick, the Florida platform, the platform on which the Great Barrier Reef is growing, and the Maldiveatolls. All these carbonate platforms and their associated reefs are confined to tropical latitudes. Today’s reefs are built mainly by scleractinian corals, but in the distant past other organisms, like archaeocyatha (during the Cambrian) or extinct cnidaria (tabulata and rugosa) were important reef builders.
Subject: Geology
Paper: Sedimentology and Petroleum Geology
Module: Carbonate platform
Content Writer: Prof. P. P Chakraborty
published: 11 Sep 2017
Carbonate Platforms (Sedimentology), Lecture by Lawrence Kanyan
This lecture covers the different types of carbonate platforms.The topic is extremely important for students preparing for GATE, NET, UPSC GSI, JAM, IFS optional, UPSC CSE optional examinations.
Please follow or page: https://www.facebook.com/planet.geology/
published: 03 Apr 2020
2.2 Carbonate Platforms [Part A]
A three part class on the distribution of sediments on modern carbonate platforms.
published: 10 Dec 2020
24 - Carbonate platforms
Distribution of facies on carbonate platforms; rimmed vs. unrimmed platforms; cross-bedded shoal facies; autocyclic and allocyclic models for genesis of meter-scale cycles
published: 25 May 2015
Deep Carbon Modelling: Carbonate Platform Accumulation, 410 - 0 Ma
Tectonic reconstruction of the accumulative deposition of reefal and carbonate platforms from 410 Ma to present day using the Matthews et al. (2016) plate model.
Animations were produced for Pall et al. (2018) and the DCO-funded project, 'Spatio-temporal modelling of deep time atmospheric carbon flux from subduction zone interactions with carbonate platforms.'
published: 01 Jun 2018
Shallow Carbonate Depositional Systems
This educational (non-profit) video was produced by a student for the Sedimentology & Stratigraphy course (GEO 224) at Cornell College.
published: 23 Sep 2020
Forces Shaping the Incredible Steep Slopes of Carbonate Platforms
The ability to build very steep slopes is a characteristics of carbonate platforms. Microbially mediated fusing of grains and subsequent prismatic early cementation construct the margins of these edifices that are often obstacles for ocean currents along continental margins. Rock fall, margin collapse, slope canyons and slope failures are common features of carbonate slopes but cascading density currents as well as bottom and surface currents also shape the sediment distribution on the slope and in the adjacent basin. Depositional slope models largely ignore the current-related deposition. The talk will illustrate the extreme height of carbonate escarpments and the related processes using the carbonate platforms in the Florida Bahamas region.
published: 27 Mar 2022
A Redox-Based Model for Carbonate Platform Drowning and Ocean Anoxic Events
Speaker: Dr. Ben Smith, Postdoctoral Scholar, Caltech University
The deposition of marine carbonate rocks is influenced by climate and seawater chemistry. Carbonate platforms usually keep pace with subsidence and sea level, but ’platform drowning’ occurs when carbonate sedimentation slows or when siliciclastics replace carbonates. Identifying specific mechanism(s) behind platform drowning is critical for understanding global environmental changes such as Ocean Anoxic Events (OAES). We developed a model for OAEs which couples ocean basin redox processes to rates of carbonate sedimentation. Through anaerobic metabolisms, deep-ocean anoxia reduces adjusts the oceans’ delicate balance between carbonate precipitation and dissolution. This quasi-steady state response acts over long timescales ...
published: 28 Sep 2021
Evolution of Isolated Carbonate Buildups
published: 08 Aug 2018
2.2 Carbonate Platforms [Part C]
A three part class on the distribution of sediments on modern carbonate platforms.
This lecture covers the different types of carbonate platforms.The topic is extremely important for students preparing for GATE, NET, UPSC GSI, JAM, IFS optiona...
This lecture covers the different types of carbonate platforms.The topic is extremely important for students preparing for GATE, NET, UPSC GSI, JAM, IFS optional, UPSC CSE optional examinations.
Please follow or page: https://www.facebook.com/planet.geology/
This lecture covers the different types of carbonate platforms.The topic is extremely important for students preparing for GATE, NET, UPSC GSI, JAM, IFS optional, UPSC CSE optional examinations.
Please follow or page: https://www.facebook.com/planet.geology/
Distribution of facies on carbonate platforms; rimmed vs. unrimmed platforms; cross-bedded shoal facies; autocyclic and allocyclic models for genesis of meter-s...
Distribution of facies on carbonate platforms; rimmed vs. unrimmed platforms; cross-bedded shoal facies; autocyclic and allocyclic models for genesis of meter-scale cycles
Distribution of facies on carbonate platforms; rimmed vs. unrimmed platforms; cross-bedded shoal facies; autocyclic and allocyclic models for genesis of meter-scale cycles
Tectonic reconstruction of the accumulative deposition of reefal and carbonate platforms from 410 Ma to present day using the Matthews et al. (2016) plate model...
Tectonic reconstruction of the accumulative deposition of reefal and carbonate platforms from 410 Ma to present day using the Matthews et al. (2016) plate model.
Animations were produced for Pall et al. (2018) and the DCO-funded project, 'Spatio-temporal modelling of deep time atmospheric carbon flux from subduction zone interactions with carbonate platforms.'
Tectonic reconstruction of the accumulative deposition of reefal and carbonate platforms from 410 Ma to present day using the Matthews et al. (2016) plate model.
Animations were produced for Pall et al. (2018) and the DCO-funded project, 'Spatio-temporal modelling of deep time atmospheric carbon flux from subduction zone interactions with carbonate platforms.'
The ability to build very steep slopes is a characteristics of carbonate platforms. Microbially mediated fusing of grains and subsequent prismatic early cementa...
The ability to build very steep slopes is a characteristics of carbonate platforms. Microbially mediated fusing of grains and subsequent prismatic early cementation construct the margins of these edifices that are often obstacles for ocean currents along continental margins. Rock fall, margin collapse, slope canyons and slope failures are common features of carbonate slopes but cascading density currents as well as bottom and surface currents also shape the sediment distribution on the slope and in the adjacent basin. Depositional slope models largely ignore the current-related deposition. The talk will illustrate the extreme height of carbonate escarpments and the related processes using the carbonate platforms in the Florida Bahamas region.
The ability to build very steep slopes is a characteristics of carbonate platforms. Microbially mediated fusing of grains and subsequent prismatic early cementation construct the margins of these edifices that are often obstacles for ocean currents along continental margins. Rock fall, margin collapse, slope canyons and slope failures are common features of carbonate slopes but cascading density currents as well as bottom and surface currents also shape the sediment distribution on the slope and in the adjacent basin. Depositional slope models largely ignore the current-related deposition. The talk will illustrate the extreme height of carbonate escarpments and the related processes using the carbonate platforms in the Florida Bahamas region.
Speaker: Dr. Ben Smith, Postdoctoral Scholar, Caltech University
The deposition of marine carbonate rocks is influenced by climate and seawater chemistry. Car...
Speaker: Dr. Ben Smith, Postdoctoral Scholar, Caltech University
The deposition of marine carbonate rocks is influenced by climate and seawater chemistry. Carbonate platforms usually keep pace with subsidence and sea level, but ’platform drowning’ occurs when carbonate sedimentation slows or when siliciclastics replace carbonates. Identifying specific mechanism(s) behind platform drowning is critical for understanding global environmental changes such as Ocean Anoxic Events (OAES). We developed a model for OAEs which couples ocean basin redox processes to rates of carbonate sedimentation. Through anaerobic metabolisms, deep-ocean anoxia reduces adjusts the oceans’ delicate balance between carbonate precipitation and dissolution. This quasi-steady state response acts over long timescales and helps explain long-lived, spatially diverse patterns of platform drowning during Mesozoic OAEs and other Phanerozoic hyperthermal events.
Speaker: Dr. Ben Smith, Postdoctoral Scholar, Caltech University
The deposition of marine carbonate rocks is influenced by climate and seawater chemistry. Carbonate platforms usually keep pace with subsidence and sea level, but ’platform drowning’ occurs when carbonate sedimentation slows or when siliciclastics replace carbonates. Identifying specific mechanism(s) behind platform drowning is critical for understanding global environmental changes such as Ocean Anoxic Events (OAES). We developed a model for OAEs which couples ocean basin redox processes to rates of carbonate sedimentation. Through anaerobic metabolisms, deep-ocean anoxia reduces adjusts the oceans’ delicate balance between carbonate precipitation and dissolution. This quasi-steady state response acts over long timescales and helps explain long-lived, spatially diverse patterns of platform drowning during Mesozoic OAEs and other Phanerozoic hyperthermal events.
This lecture covers the different types of carbonate platforms.The topic is extremely important for students preparing for GATE, NET, UPSC GSI, JAM, IFS optional, UPSC CSE optional examinations.
Please follow or page: https://www.facebook.com/planet.geology/
Distribution of facies on carbonate platforms; rimmed vs. unrimmed platforms; cross-bedded shoal facies; autocyclic and allocyclic models for genesis of meter-scale cycles
Tectonic reconstruction of the accumulative deposition of reefal and carbonate platforms from 410 Ma to present day using the Matthews et al. (2016) plate model.
Animations were produced for Pall et al. (2018) and the DCO-funded project, 'Spatio-temporal modelling of deep time atmospheric carbon flux from subduction zone interactions with carbonate platforms.'
The ability to build very steep slopes is a characteristics of carbonate platforms. Microbially mediated fusing of grains and subsequent prismatic early cementation construct the margins of these edifices that are often obstacles for ocean currents along continental margins. Rock fall, margin collapse, slope canyons and slope failures are common features of carbonate slopes but cascading density currents as well as bottom and surface currents also shape the sediment distribution on the slope and in the adjacent basin. Depositional slope models largely ignore the current-related deposition. The talk will illustrate the extreme height of carbonate escarpments and the related processes using the carbonate platforms in the Florida Bahamas region.
Speaker: Dr. Ben Smith, Postdoctoral Scholar, Caltech University
The deposition of marine carbonate rocks is influenced by climate and seawater chemistry. Carbonate platforms usually keep pace with subsidence and sea level, but ’platform drowning’ occurs when carbonate sedimentation slows or when siliciclastics replace carbonates. Identifying specific mechanism(s) behind platform drowning is critical for understanding global environmental changes such as Ocean Anoxic Events (OAES). We developed a model for OAEs which couples ocean basin redox processes to rates of carbonate sedimentation. Through anaerobic metabolisms, deep-ocean anoxia reduces adjusts the oceans’ delicate balance between carbonate precipitation and dissolution. This quasi-steady state response acts over long timescales and helps explain long-lived, spatially diverse patterns of platform drowning during Mesozoic OAEs and other Phanerozoic hyperthermal events.
A carbonate platform is a sedimentary body which possesses topographic relief, and is composed of autochthonous calcareous deposits (Wilson, 1975). Platform growth is mediated by sessile organisms whose skeletons build up the reef or by organisms (usually microbes) which induce carbonate precipitation through their metabolism. Therefore, carbonate platforms can not grow up everywhere: they are not present in places where limiting factors to the life of reef-building organisms exist. Such limiting factors are, among others: light, watertemperature, transparency and pH-Value. For example, carbonate sedimentation along the AtlanticSouth American coasts takes place everywhere but at the mouth of the Amazon River, because of the intense turbidity of the water there (Carannante et al., 1988). Spectacular examples of present-day carbonate platforms are the Bahama Banks under which the platform is roughly 8km thick, the Yucatan Peninsula which is up to 2km thick, the Florida platform, the platform on which the Great Barrier Reef is growing, and the Maldiveatolls. All these carbonate platforms and their associated reefs are confined to tropical latitudes. Today’s reefs are built mainly by scleractinian corals, but in the distant past other organisms, like archaeocyatha (during the Cambrian) or extinct cnidaria (tabulata and rugosa) were important reef builders.
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