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...
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Autor*in:	Carniti, Alessandro P. [verfasserIn] Della Porta, Giovanna Banks, Vanessa J. Stephenson, Michael H. Angiolini, Lucia

Format:	Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	Mississippian Visean Mud mound Reef Brachiopod Derbyshire

Anmerkung:	© The Author(s) 2023

Übergeordnetes Werk:	Enthalten in: Facies - Springer Berlin Heidelberg, 1979, 69(2023), 2 vom: Apr.
Übergeordnetes Werk:	volume:69 ; year:2023 ; number:2 ; month:04

Links:	Volltext

DOI / URN:	10.1007/s10347-023-00663-w

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.
650		4	\|a Mississippian
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700	1		\|a Angiolini, Lucia \|0 (orcid)0000-0003-0778-5771 \|4 aut
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allfields	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
spelling	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
allfields_unstemmed	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
allfieldsGer	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
allfieldsSound	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
language	English
source	Enthalten in Facies 69(2023), 2 vom: Apr. volume:69 year:2023 number:2 month:04
sourceStr	Enthalten in Facies 69(2023), 2 vom: Apr. volume:69 year:2023 number:2 month:04
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Mississippian Visean Mud mound Reef Brachiopod Derbyshire
dewey-raw	550
isfreeaccess_bool	false
container_title	Facies
authorswithroles_txt_mv	Carniti, Alessandro P. @@aut@@ Della Porta, Giovanna @@aut@@ Banks, Vanessa J. @@aut@@ Stephenson, Michael H. @@aut@@ Angiolini, Lucia @@aut@@
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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. 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author	Carniti, Alessandro P.
spellingShingle	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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topic_title	550 VZ 13 ssgn Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth Mississippian Visean Mud mound Reef Brachiopod Derbyshire
topic	ddc 550 ssgn 13 misc Mississippian misc Visean misc Mud mound misc Reef misc Brachiopod misc Derbyshire
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title	Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth
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title_full	Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth
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author_browse	Carniti, Alessandro P. Della Porta, Giovanna Banks, Vanessa J. Stephenson, Michael H. Angiolini, Lucia
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title_sort	revisiting the upper visean mud mounds from derbyshire (uk): the role of brachiopods in their growth
title_auth	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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title_short	Revisiting the upper Visean mud mounds from Derbyshire (UK): the role of brachiopods in their growth
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