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Great Bank of Guizhou

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Journal Article

The Late Permian to Late Triassic Great Bank of Guizhou: An isolated carbonate platform in the Nanpanjiang Basin of Guizhou Province, China

Brian M. Kelley, Daniel J. Lehrmann, Meiyi Yu, Marcello Minzoni, Paul Enos, Xiaowei Li, Kimberly V. Lau, Jonathan L. Payne
Journal: AAPG Bulletin
Published: 01 April 2017
AAPG Bulletin (2017) 101 (4): 553–562.
DOI: https://doi.org/10.1306/011817DIG17034
...Brian M. Kelley; Daniel J. Lehrmann; Meiyi Yu; Marcello Minzoni; Paul Enos; Xiaowei Li; Kimberly V. Lau; Jonathan L. Payne ABSTRACT The Late Permian to Late Triassic Great Bank of Guizhou (GBG) in southwest China is one of the few isolated carbonate platforms in the world that exposes...
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View PDF for article title, The Late Permian to Late Triassic <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span>: An isolated carbonate platform in the Nanpanjiang Basin of <span class="search-highlight">Guizhou</span> Province, China
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Journal Article

ENVIRONMENTAL AND BIOLOGICAL CONTROLS ON THE INITIATION AND GROWTH OF A MIDDLE TRIASSIC (ANISIAN) REEF COMPLEX ON THE GREAT BANK OF GUIZHOU, GUIZHOU PROVINCE, CHINA

JONATHAN L. PAYNE, DANIEL J. LEHRMANN, SHANNON CHRISTENSEN, JIAYONG WEI, ANDREW H. KNOLL
Journal: PALAIOS
Published: 01 August 2006
PALAIOS (2006) 21 (4): 325–343.
DOI: https://doi.org/10.2110/palo.2005.P05-58e
...JONATHAN L. PAYNE; DANIEL J. LEHRMANN; SHANNON CHRISTENSEN; JIAYONG WEI; ANDREW H. KNOLL Abstract The Great Bank of Guizhou (GBG) is an isolated Late Permian to Late Triassic carbonate platform in the Nanpanjiang Basin of Guizhou Province, southwest China. A faulted syncline exposes a cross section...
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View PDF for article title, ENVIRONMENTAL AND BIOLOGICAL CONTROLS ON THE INITIATION AND GROWTH OF A MIDDLE TRIASSIC (ANISIAN) REEF COMPLEX ON THE <span class="search-highlight">GREAT</span> <span class="search-highlight">BANK</span> OF <span class="search-highlight">GUIZHOU</span>, <span class="search-highlight">GUIZHOU</span> PROVINCE, CHINA
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Add to Citation Manager for ENVIRONMENTAL AND BIOLOGICAL CONTROLS ON THE INITIATION AND GROWTH OF A MIDDLE TRIASSIC (ANISIAN) REEF COMPLEX ON THE <span class="search-highlight">GREAT</span> <span class="search-highlight">BANK</span> OF <span class="search-highlight">GUIZHOU</span>, <span class="search-highlight">GUIZHOU</span> PROVINCE, CHINA
Journal Article

The Pattern and Timing of Biotic Recovery from the End-Permian Extinction on the Great Bank of Guizhou, Guizhou Province, China

JONATHAN L. PAYNE, DANIEL J. LEHRMANN, JIAYONG WEI, ANDREW H. KNOLL
Journal: PALAIOS
Published: 01 February 2006
PALAIOS (2006) 21 (1): 63–85.
DOI: https://doi.org/10.2110/palo.2005.p05-12p
... extinction on the Great Bank of Guizhou (GBG)—an isolated Late Permian to Late Triassic carbonate platform in south China. Exposure of a two-dimensional cross-section of the platform permits the comparison of faunal patterns along an environmental gradient from shallow to deep water. The diverse Late Permian...
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View PDF for article title, The Pattern and Timing of Biotic Recovery from the End-Permian Extinction on the <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span>, <span class="search-highlight">Guizhou</span> Province, China
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Add to Citation Manager for The Pattern and Timing of Biotic Recovery from the End-Permian Extinction on the <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span>, <span class="search-highlight">Guizhou</span> Province, China
Journal Article

Metazoan-algal benthic ecosystems enhance automicritic slope boundstone: The Triassic Great Bank of Guizhou carbonate platform, Xiliang margin, China

Brian M. Kelley, Daniel J. Lehrmann, Meiyi Yu, Kimberly V. Lau, Demir Altiner, Marcello Minzoni, Paul Enos, Xiaowei Li, Jonathan L. Payne
Journal: AAPG Bulletin
Published: 01 October 2024
AAPG Bulletin (2024) 108 (10): 1851–1884.
DOI: https://doi.org/10.1306/06112422064
... recovery on the Xiliang slope of the Great Bank of Guizhou (GBG), an isolated carbonate platform in southern China. Our findings indicate that automicritic boundstone accumulation was not enhanced by depleted Early Triassic benthic ecosystems. Instead, detrital sediment dominated the GBG slope...
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View PDF for article title, Metazoan-algal benthic ecosystems enhance automicritic slope boundstone: The Triassic <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span> carbonate platform, Xiliang margin, China
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Add to Citation Manager for Metazoan-algal benthic ecosystems enhance automicritic slope boundstone: The Triassic <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span> carbonate platform, Xiliang margin, China
Journal Article

Triassic Foraminifera from the Great Bank of Guizhou, Nanpanjiang Basin, south China: taxonomic account, biostratigraphy, and implications for recovery from end-Permian mass extinction

Demir Altıner, Jonathan L. Payne, Daniel J. Lehrmann, Sevinç Özkan-Altıner, Brian M. Kelley, Mindi M. Summers, Meiyi Yu
Published: 01 December 2021
Journal of Paleontology (2021) 95 (S84): 1–53.
DOI: https://doi.org/10.1017/jpa.2021.10
... into the Mesozoic history of this group. Here we report the calcareous and agglutinated foraminifera recovered from five measured stratigraphic sections on the Great Bank of Guizhou, an uppermost Permian to Upper Triassic isolated carbonate platform in the Nanpanjiang Basin, south China. The material contains...
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View PDF for article title, Triassic Foraminifera from the <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span>, Nanpanjiang Basin, south China: taxonomic account, biostratigraphy, and implications for recovery from end-Permian mass extinction
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Add to Citation Manager for Triassic Foraminifera from the <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span>, Nanpanjiang Basin, south China: taxonomic account, biostratigraphy, and implications for recovery from end-Permian mass extinction
Journal Article

Controls on facies architecture of a large Triassic carbonate platform; the Great Bank of Guizhou, Nanpanjiang Basin, South China

Daniel J. Lehrmann, Wei Jiayong, Paul Enos
Published: 01 March 1998
Journal of Sedimentary Research (1998) 68 (2): 311–326.
DOI: https://doi.org/10.2110/jsr.68.311
...Daniel J. Lehrmann; Wei Jiayong; Paul Enos Abstract The Great Bank of Guizhou (GBG) is an exceptionally well exposed isolated Triassic platform in the Nanpanjiang Basin of South China. The platform is exhumed with its depositional profile preserved and is dissected by a faulted syncline...
View PDF for article title, Controls on facies architecture of a large Triassic carbonate platform; the <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span>, Nanpanjiang Basin, South China
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Add to Citation Manager for Controls on facies architecture of a large Triassic carbonate platform; the <span class="search-highlight">Great</span> <span class="search-highlight">Bank</span> of <span class="search-highlight">Guizhou</span>, Nanpanjiang Basin, South China
Image
The Great Bank of Guizhou, Xiliang margin. Location indicated in schematic at upper right of (A). (A) Locations of measured sections (green lines and text), figure numbers of photographed samples and outcrops (orange text and arrows), field-based bedding attitude measurements (white), and bedding traces on the satellite imagery (solid yellow lines). Ikonos satellite imagery (80 cm/pixel). (B) Interpretation of platform development stages. The ages and platform geometry are presented in Table 1. Facies types and descriptions are presented in Table 2. (C) Exposure of the eastern syncline limb. Location and direction of viewpoint are indicated by the purple arrow in (A). High-relief topography in the foreground and middle ground is the Xiliang platform carbonate. Buildings in the syncline axis are on younger (Carnian), basin-filling siliciclastics.

The Great Bank of Guizhou, Xiliang margin. Location indicated in schematic ...

Published: 01 October 2024
Figure 3. The Great Bank of Guizhou, Xiliang margin. Location indicated in schematic at upper right of (A). (A) Locations of measured sections (green lines and text), figure numbers of photographed samples and outcrops (orange text and arrows), field-based bedding attitude measurements (white
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Pre-Great Bank of Guizhou lithofacies. Uppermost Permian. Eastern syncline limb. (A) Fossiliferous packstone to grainstone containing fusulinid foraminifers, brachiopods, mollusks, sponges, and calcareous algae. Facies 1. (B) Siliceous mudstone with bedded chert. Facies 2.

Pre-Great Bank of Guizhou lithofacies. Uppermost Permian. Eastern syncline ...

Published: 01 October 2024
Figure 6. Pre-Great Bank of Guizhou lithofacies. Uppermost Permian. Eastern syncline limb. (A) Fossiliferous packstone to grainstone containing fusulinid foraminifers, brachiopods, mollusks, sponges, and calcareous algae. Facies 1. (B) Siliceous mudstone with bedded chert. Facies 2.
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Reconstruction of key development stages of the Great Bank of Guizhou at Bianyang with vertical exaggeration removed. Modified from Kelley (2014). (A) Initiation and low-relief bank stages. (B) Aggrading and steepening stage. (C) Prograding reef stage. (D) High-relief escarpment stage.

Reconstruction of key development stages of the Great Bank of Guizhou at Bi...

Published: 01 April 2017
Figure 3. Reconstruction of key development stages of the Great Bank of Guizhou at Bianyang with vertical exaggeration removed. Modified from Kelley (2014) . (A) Initiation and low-relief bank stages. (B) Aggrading and steepening stage. (C) Prograding reef stage. (D) High-relief escarpment stage.
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Detailed geologic maps. A) Great Bank of Guizhou (GBG). B) The Pingguo area of the Chongzuo‐Pingguo platform (CPP). Locations of maps are shown in Figure 1. Field localities are as follows: RB = Rungbao, LB = Langbai, DJ = Dajiang, HP = Heping, DW = Dawen, DJW = Dongjiawan, XB = Xinbaihou, HC = Hochang, LL = Longlan, TP = Taiping, NY = Naying, TG = Tangneng.

Detailed geologic maps. A ) Great Bank of Guizhou (GBG). B ) The Pingguo ...

Published: 01 July 2015
Fig. 2.— Detailed geologic maps. A ) Great Bank of Guizhou (GBG). B ) The Pingguo area of the Chongzuo‐Pingguo platform (CPP). Locations of maps are shown in Figure 1 . Field localities are as follows: RB = Rungbao, LB = Langbai, DJ = Dajiang, HP = Heping, DW = Dawen, DJW = Dongjiawan, XB
Image
Macroscopic characteristics of oolites from the Great Bank of Guizhou (GBG). (A) Outcrop photograph of dolomitized oolite with herringbone cross-beds in the lower part of the platform interior dolo-oolite at the Dajiang section. Reversing current directions indicating tidal currents. The scale bar on the lower left is 10 cm (4 in.). (B) Oolite grainstone with ooids ranging up to 5 mm and rounded coated intraclasts up to 1 cm (0.4 in.). From the interior of the GBG, proximal to the southern margin, south of Dawen ( Figure 2 for location). (C) Supratidal fenestral laminite facies containing ooids and rounded oolite intraclasts (black arrows). Note fenestral pores, dissolved ooids with dropped nuclei (white arrows), and well-preserved ooids truncated at margins of intraclast. From the upper part of dolo-oolite unit in platform interior at Dajiang ( Figures 2, 7 for location). (D) Oolite fabric expressed on weathered surface of coarsely crystalline dolomite, ramp crest shoals on the northern margin of the GBG at Xiliang ( Figure 2 for location). (E) Outcrop photograph of ripple forms in cross section in oolite from shoals on the southern margin at Louhua ( Figure 2 for location).

Macroscopic characteristics of oolites from the Great Bank of Guizhou (GBG)...

Published: 01 August 2012
Figure 8 Macroscopic characteristics of oolites from the Great Bank of Guizhou (GBG). (A) Outcrop photograph of dolomitized oolite with herringbone cross-beds in the lower part of the platform interior dolo-oolite at the Dajiang section. Reversing current directions indicating tidal currents
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Stratigraphic correlation between Meishan and the Great Bank of Guizhou (GBG), illustrating local discordance in conodont ranges implied by correlation based upon the mass-extinction horizon and δ13C stratigraphy. Conodont ranges as reported by Payne et al. (2007), Jiang et al. (2007), and Ezaki et al. (2008). Conodont zones for Meishan follow Jiang et al. (2007). Schematic carbon isotope curves based upon data from Jin et al. (2000), Krull et al. (2004), Payne et al. (2004), and Xie et al. (2007). H.—Hindeodus; C.—Clarkina; I.—Isarcicella; VPDB—Vienna Peedee Belemnite.

Stratigraphic correlation between Meishan and the Great Bank of Guizhou (GB...

Published: 01 May 2009
Figure 1. Stratigraphic correlation between Meishan and the Great Bank of Guizhou (GBG), illustrating local discordance in conodont ranges implied by correlation based upon the mass-extinction horizon and δ 13 C stratigraphy. Conodont ranges as reported by Payne et al. (2007) , Jiang et al
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Restored cross sections of the Great Bank of Guizhou illustrating Late Permian to Late Triassic evolution. Cross section is from the northwest-trending syncline that dissects the platform (Figure 3 for location). For stratigraphic data, see Lehrmann et al. (1998). (A) Lower Triassic: low-relief bank stage; (B) Anisian–early Ladinian: aggrading reef-rimmed stage. (C) Ladinian: high-relief escarpment stage. (D) Carnian: termination (drowning). Sb = sequence boundary; F = flooding surface; Max-F = maximum flooding surface.

Restored cross sections of the Great Bank of Guizhou illustrating Late Perm...

Published: 01 March 2007
Figure 15 Restored cross sections of the Great Bank of Guizhou illustrating Late Permian to Late Triassic evolution. Cross section is from the northwest-trending syncline that dissects the platform ( Figure 3 for location). For stratigraphic data, see Lehrmann et al. (1998) . (A) Lower Triassic
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FIGURE 6—Basal Triassic facies in the Great Bank of Guizhou. See Fig. 2A for locations. Fossil types indicated as follows: g=gastropod, b=bivalve, f=fusulinid, r=Renalcis. (A) Close up of wavy bedding with stromatolitic appearance in calcimicrobial framestone at Dajiang. Hammer for scale. (B) Slab of calcimicrobial framestone from Dajiang. Darker colored framework is composed of calcified globular, tufted, and dendritic structures similar to Renalcis (r) that enclose irregular network of internal cavities partly filled with internal sediment (s). See Lehrmann (1999) for petrographic details of this facies. (C) Polished slab of the PTB from Langbai. Scale bar in centimeters. PTB event horizon is represented by abrupt change (white line) at the boundary between the skeletal packstone of the Wujiaping Formatation (lower) and calcimicrobial framestone (upper). Small spherical white grains in the packstone (lower) are Palaeofusulina (f). The calcimicrobial framestone (upper) is composed of calcified black globular fossils (r) surrounding lighter-colored irregular internal cavities. (D) Thin section of molluscan grainstone from Heping. Note that most shells are randomly oriented and preserved only as thin micritic envelopes filled with sparry calcite (arrows). Scale is 1 mm. (E) Thin section of molluscan grainstone from Heping. Note micrite (arrows) and peloidal internal sediment perched above bivalve shells (b). Scale is 1 mm. (F) Thin section of microgastropod packstone from Heping. Note dark micrite filling most gastropods shells (g). Scale is 1 mm

FIGURE 6 —Basal Triassic facies in the Great Bank of Guizhou. See Fig. 2A ...

Published: 01 April 2003
FIGURE 6 —Basal Triassic facies in the Great Bank of Guizhou. See Fig. 2A for locations. Fossil types indicated as follows: g=gastropod, b=bivalve, f=fusulinid, r= Renalcis . (A) Close up of wavy bedding with stromatolitic appearance in calcimicrobial framestone at Dajiang. Hammer for scale. (B
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Geologic setting. (A) Early and Middle Triassic paleogeography and location of the South China Block. Modified from Scotese (2014). (B) Present location of the Nanpanjiang Basin in southern China. (C) Detail of the Early Triassic Nanpanjiang Basin showing the Yangtze Platform, the Great Bank of Guizhou, other isolated platforms within the basin, and the Jiangnan Massif. Extent of view indicated by red box in (B). (D) Detail of the Great Bank of Guizhou. Red box indicates study area. Modified from Kelley et al. (2017).

Geologic setting. (A) Early and Middle Triassic paleogeography and location...

Published: 01 October 2024
, the Great Bank of Guizhou, other isolated platforms within the basin, and the Jiangnan Massif. Extent of view indicated by red box in (B). (D) Detail of the Great Bank of Guizhou. Red box indicates study area. Modified from Kelley et al. (2017) .
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Geologic setting. (A) Paleogeographic map showing approximate location (in black) of the South China Block during the Late Permian to Triassic. Modified from Payne et al. (2006b). (B) Location of the Nanpanjiang Basin in south China (red box). (C) Detailed view of the Nanpanjiang Basin with the position of the Great Bank of Guizhou indicated. View is of the location enclosed by the red box in (B). (D) Detailed view of the Great Bank of Guizhou, with the location of Bianyang and the Bianyang Syncline indicated. View is of the location enclosed by the red box in (C). Red box near Bianyang indicates the location and geographic extent of the facies map in Figure 2. (E) Escarpment of the Great Bank of Guizhou. Stratigraphic top is to right; structural dip of approximately 65°. The platform margin erosional escarpment is represented by the sharp contact between platform carbonates and siliciclastic turbidites of the Bianyang Formation (foreground). UTM = Universal Transverse Mercator.

Geologic setting. (A) Paleogeographic map showing approximate location (in ...

Published: 01 April 2017
Basin with the position of the Great Bank of Guizhou indicated. View is of the location enclosed by the red box in (B). (D) Detailed view of the Great Bank of Guizhou, with the location of Bianyang and the Bianyang Syncline indicated. View is of the location enclosed by the red box in (C). Red box near
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Petrographic characteristics of platform-margin oolite grainstone facies. (A, B) Ooid lime grainstone with giant ooids from the southern margin of the Great Bank of Guizhou at Bangeng ( Figure 2 for location). (A) Contains ooids up to 1 cm (0.4 in.) and composite coated grains more than 2 cm (0.8 in.) across. (B) Contains ooids with consistent size 7 to 8 mm in diameter. (C) Oolitic grainstone with ooids up to 3 mm and composite coated grains from the northern margin of the Great Bank of Guizhou, Xiliang area. Note the alternation of micritic cortical layers with a detailed fabric preservation and sparry layers with destroyed fabrics and brittle compaction of adjacent layers (arrows). Sparry layers are interpreted to have originally been aragonite. (D) Oolitic lime grainstone with rounded intraclasts and composite coated grains showing an evidence of repeated abrasion and recoating. Arrows indicate alternation of cortices with fabric-destructive sparry layers (original aragonite) and micrite layers (calcite). Southern margin of the Great Bank of Guizhou, Bangeng area.

Petrographic characteristics of platform-margin oolite grainstone facies. (...

Published: 01 August 2012
Figure 14 Petrographic characteristics of platform-margin oolite grainstone facies. (A, B) Ooid lime grainstone with giant ooids from the southern margin of the Great Bank of Guizhou at Bangeng ( Figure 2 for location). (A) Contains ooids up to 1 cm (0.4 in.) and composite coated grains more
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Figure1—Locations of the Dajiang and Bianyang sections, southern Guizhou Province, Southwest China. Early Triassic paleogeographic map of the Great Bank of Guizhou as modified from Lehrmann et al. (2001)

Figure 1 —Locations of the Dajiang and Bianyang sections, southern Guizhou...

Published: 01 September 2009
Figure 1 —Locations of the Dajiang and Bianyang sections, southern Guizhou Province, Southwest China. Early Triassic paleogeographic map of the Great Bank of Guizhou as modified from Lehrmann et al. (2001)
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Middle Triassic (Ladinian) lithofacies and interpreted paleogeography of the Nanpanjiang Basin and Yangtze platform in Guizhou, Guangxi, and Yunnan. Compilation data and methods are given in the caption of Figure 3. GBG = Great Bank of Guizhou.

Middle Triassic (Ladinian) lithofacies and interpreted paleogeography of th...

Published: 01 March 2007
Figure 5 Middle Triassic (Ladinian) lithofacies and interpreted paleogeography of the Nanpanjiang Basin and Yangtze platform in Guizhou, Guangxi, and Yunnan. Compilation data and methods are given in the caption of Figure 3 . GBG = Great Bank of Guizhou.
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Middle Triassic (Anisian) lithofacies and interpreted paleogeography of the Nanpanjiang Basin and Yangtze platform in Guizhou, Guangxi, and Yunnan. Compilation data and methods are given in the caption of Figure 3. GBG = Great Bank of Guizhou.

Middle Triassic (Anisian) lithofacies and interpreted paleogeography of the...

Published: 01 March 2007
Figure 4 Middle Triassic (Anisian) lithofacies and interpreted paleogeography of the Nanpanjiang Basin and Yangtze platform in Guizhou, Guangxi, and Yunnan. Compilation data and methods are given in the caption of Figure 3 . GBG = Great Bank of Guizhou.