Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth
Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition...
Ausführliche Beschreibung
Autor*in: |
Carniti, Alessandro P. [verfasserIn] |
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Artikel |
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Sprache: |
Englisch |
Erschienen: |
2023 |
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Anmerkung: |
© The Author(s) 2023 |
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Übergeordnetes Werk: |
Enthalten in: Facies - Springer Berlin Heidelberg, 1979, 69(2023), 2 vom: Apr. |
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Übergeordnetes Werk: |
volume:69 ; year:2023 ; number:2 ; month:04 |
Links: |
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DOI / URN: |
10.1007/s10347-023-00663-w |
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Katalog-ID: |
OLC2134674296 |
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520 | |a Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. | ||
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10.1007/s10347-023-00663-w doi (DE-627)OLC2134674296 (DE-He213)s10347-023-00663-w-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Carniti, Alessandro P. verfasserin (orcid)0000-0002-9590-1615 aut Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. Mississippian Visean Mud mound Reef Brachiopod Derbyshire Della Porta, Giovanna (orcid)0000-0003-3479-0592 aut Banks, Vanessa J. (orcid)0000-0001-6335-7080 aut Stephenson, Michael H. (orcid)0000-0002-9881-1578 aut Angiolini, Lucia (orcid)0000-0003-0778-5771 aut Enthalten in Facies Springer Berlin Heidelberg, 1979 69(2023), 2 vom: Apr. (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:69 year:2023 number:2 month:04 https://doi.org/10.1007/s10347-023-00663-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_188 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2173 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 AR 69 2023 2 04 |
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10.1007/s10347-023-00663-w doi (DE-627)OLC2134674296 (DE-He213)s10347-023-00663-w-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Carniti, Alessandro P. verfasserin (orcid)0000-0002-9590-1615 aut Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. Mississippian Visean Mud mound Reef Brachiopod Derbyshire Della Porta, Giovanna (orcid)0000-0003-3479-0592 aut Banks, Vanessa J. (orcid)0000-0001-6335-7080 aut Stephenson, Michael H. (orcid)0000-0002-9881-1578 aut Angiolini, Lucia (orcid)0000-0003-0778-5771 aut Enthalten in Facies Springer Berlin Heidelberg, 1979 69(2023), 2 vom: Apr. (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:69 year:2023 number:2 month:04 https://doi.org/10.1007/s10347-023-00663-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_188 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2173 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 AR 69 2023 2 04 |
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10.1007/s10347-023-00663-w doi (DE-627)OLC2134674296 (DE-He213)s10347-023-00663-w-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Carniti, Alessandro P. verfasserin (orcid)0000-0002-9590-1615 aut Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. Mississippian Visean Mud mound Reef Brachiopod Derbyshire Della Porta, Giovanna (orcid)0000-0003-3479-0592 aut Banks, Vanessa J. (orcid)0000-0001-6335-7080 aut Stephenson, Michael H. (orcid)0000-0002-9881-1578 aut Angiolini, Lucia (orcid)0000-0003-0778-5771 aut Enthalten in Facies Springer Berlin Heidelberg, 1979 69(2023), 2 vom: Apr. (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:69 year:2023 number:2 month:04 https://doi.org/10.1007/s10347-023-00663-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_188 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2173 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 AR 69 2023 2 04 |
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10.1007/s10347-023-00663-w doi (DE-627)OLC2134674296 (DE-He213)s10347-023-00663-w-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Carniti, Alessandro P. verfasserin (orcid)0000-0002-9590-1615 aut Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. Mississippian Visean Mud mound Reef Brachiopod Derbyshire Della Porta, Giovanna (orcid)0000-0003-3479-0592 aut Banks, Vanessa J. (orcid)0000-0001-6335-7080 aut Stephenson, Michael H. (orcid)0000-0002-9881-1578 aut Angiolini, Lucia (orcid)0000-0003-0778-5771 aut Enthalten in Facies Springer Berlin Heidelberg, 1979 69(2023), 2 vom: Apr. (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:69 year:2023 number:2 month:04 https://doi.org/10.1007/s10347-023-00663-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_188 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2173 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 AR 69 2023 2 04 |
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10.1007/s10347-023-00663-w doi (DE-627)OLC2134674296 (DE-He213)s10347-023-00663-w-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Carniti, Alessandro P. verfasserin (orcid)0000-0002-9590-1615 aut Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. Mississippian Visean Mud mound Reef Brachiopod Derbyshire Della Porta, Giovanna (orcid)0000-0003-3479-0592 aut Banks, Vanessa J. (orcid)0000-0001-6335-7080 aut Stephenson, Michael H. (orcid)0000-0002-9881-1578 aut Angiolini, Lucia (orcid)0000-0003-0778-5771 aut Enthalten in Facies Springer Berlin Heidelberg, 1979 69(2023), 2 vom: Apr. (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:69 year:2023 number:2 month:04 https://doi.org/10.1007/s10347-023-00663-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_188 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2173 GBV_ILN_4082 GBV_ILN_4112 GBV_ILN_4305 AR 69 2023 2 04 |
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Carniti, Alessandro P. |
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Carniti, Alessandro P. ddc 550 ssgn 13 misc Mississippian misc Visean misc Mud mound misc Reef misc Brachiopod misc Derbyshire Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth |
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revisiting the upper visean mud mounds from derbyshire (uk): the role of brachiopods in their growth |
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Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth |
abstract |
Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. © The Author(s) 2023 |
abstractGer |
Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. © The Author(s) 2023 |
abstract_unstemmed |
Abstract Several brachiopod-rich mud mounds occur in the upper Visean (Brigantian) of the Derbyshire Carbonate Platform succession in UK. The re-evaluation of the lithofacies architecture of a Derbyshire mud mound complex, developed in an intraplatform middle-ramp environment, led to the recognition of three lithofacies associations: (a) a 10 m thick basal unit of automicrite boundstone with siliceous sponge spicules and brachiopod–bryozoan packstone to wackestone beds; (b) a 10 m thick, 250 m wide, lens-shaped, convex-up massive core of clotted peloidal micrite and fenestellid bryozoan boundstone with sponge spicules; (c) inclined brachiopod–bryozoan–crinoid packstone flank beds. In the mud mound complex core, most of the carbonate mud with clotted peloidal and structureless micrite fabric is the result of biologically induced and influenced in-situ precipitation processes (automicrite). Brachiopods are not, as previously thought, limited to storm-scoured “pockets” in the mud mound complex core but are abundant and diverse in all lithofacies and lived on the irregular mud mound complex surface concentrating in depressions sustained by automicrite boundstone and the growth of bryozoans and sponges. The upper Visean Derbyshire mud mounds are, thus, representatives of a newly defined fenestellid bryozoan–brachiopod–siliceous sponge mud mound category, occurring in various middle–upper Visean Western European sites, a sub-type of the fenestellid bryozoan–crinoid–brachiopod Type 3 buildups of Bridges et al. (1995). These mud mounds, and other types of brachiopod-rich buildups, developed in carbonate platform settings between fair-weather and storm wave base, in dysphotic environments with dispersed food resources during the Visean. Brachiopod mud mound colonisation was favoured by moderate water depth, availability of food resources, and diverse substrates. © The Author(s) 2023 |
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Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth |
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