Myriapora bugei d'Hondt 1975
Myriapora bugei d’Hondt, 1975 Fig. 4, Table 4 Myriapora bugei d’Hondt, 1975: 585, figs 23, 25-28. non Myriapora bugei – El Hajjaji 1992: 250, pl. 15, figs 14-15. Material examined Lectotype (here designated) MNHN IB-2013-3, one dried colony fragment (former part of MNHN 7481), Jean Charcot , Biaçore...
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Online Access: | https://dx.doi.org/10.5281/zenodo.3815230 https://zenodo.org/record/3815230 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
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unknown |
topic |
Biodiversity Taxonomy Animalia Bryozoa Gymnolaemata Cheilostomatida Myriaporidae Myriapora Myriapora bugei |
spellingShingle |
Biodiversity Taxonomy Animalia Bryozoa Gymnolaemata Cheilostomatida Myriaporidae Myriapora Myriapora bugei Berning, Björn Myriapora bugei d'Hondt 1975 |
topic_facet |
Biodiversity Taxonomy Animalia Bryozoa Gymnolaemata Cheilostomatida Myriaporidae Myriapora Myriapora bugei |
description |
Myriapora bugei d’Hondt, 1975 Fig. 4, Table 4 Myriapora bugei d’Hondt, 1975: 585, figs 23, 25-28. non Myriapora bugei – El Hajjaji 1992: 250, pl. 15, figs 14-15. Material examined Lectotype (here designated) MNHN IB-2013-3, one dried colony fragment (former part of MNHN 7481), Jean Charcot , Biaçores Stn 109, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17’ W, 190–230 m. Paralectotypes (here designated) MNHN 7481, Jean Charcot , Biaçores Stn 109, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17’ W, 190–230 m; MNHN IB- 2013-2, one dried colony fragment (former part of MNHN 7492), Jean Charcot , Biaçores Stn 110, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17.5’ W, 300–350 m; MNHN 7482, 13 colony fragments in ethanol, Jean Charcot , Biaçores Stn 109, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17’ W, 190–230 m; MNHN 7488, one colony fragment in ethanol, Jean Charcot , Biaçores Stn 110, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17.5’ W, 300–350 m; MNHN 7492, four colony fragments in ethanol, Jean Charcot , Biaçores Stn 110, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17.5’ W, 300– 350 m. The original material available to d’Hondt (1975: 560) was from Biaçores stations 109 and 110. However, he did not indicate type material when introducing Myriapora bugei , and the figured specimen (figs 23, 25-28) was subsequently destroyed (J.-L. d’Hondt pers. comm. 2012). For the same reasons as stated in the Material section for Cellaria harmelini (see above), the type specimens of M. bugei were invalidly considered as “ holotype ” and “ paratypes ” by Tricart & d’Hondt (2009), and are formally designated here as lectotype and paralectotypes, respectively. Description Colony erect, rigid, delicate branching, producing lateral offsets at an angle of about 90° at irregular intervals (Fig. 4A). Branches long (3-4 cm), slender and cylindrical, with the zooids opening all around. Zooids large, radially arranged in distinct whorls of 4 (rarely 5), with all orifices at same level and the distal whorl ideally alternating (Fig. 4 B-C); zooecia elongate rectangular but boundaries invisible on colony surface. Frontal shield of mature zooecia gently raising towards orifice, giving distal branches an undulating morphology that is slightly reduced due to frontal calcification during ontogeny (Fig. 4 A- C); frontal shield regularly perforated by numerous elongate pores in spindle-shaped depressions that are longitudinally aligned (Fig. 4B), surface finely granular (Fig. 4 D-E). Primary orifice dimorphic; in autozooids slightly longer than wide (Fig. 4D), anter horseshoe-shaped, widest slightly distal to middistance, proximolateral corners rounded with the short shoulders slightly sloping towards a deep and broadly U-shaped sinus occupying about two-thirds of total proximal width, condyles conspicuous, broad and with rounded edges, not extending beyond shoulders of the proximolateral margin; orifice in ovicellate zooids D-shaped (Fig. 4E), of similar length as in autozooids but especially the proximal margin distinctly broader, sinus a very shallow straight edge comprising four-fifths of total proximal width, proximolateral shoulders thus relatively short and fairly straight, condyles similar to those in autozooids; orifice becoming immersed by frontal calcification and occasionally closed during ontogeny in proximal branch regions, in which case a small short peristome with a central pore remains. No oral spines. Ovicells relatively rare, present in all zooids of certain whorls, indicated by a slightly thicker swelling of this branch region and by frontal pseudopores that are radially arranged from the proximal ooecium centre (Fig. 4B, E), ooecium mostly incorporated into frontal shields of the distal zooids, surface as frontal shield of zooecia, boundaries invisible at colony surface, ovicell aperture at an acute angle to frontal plane, closure of the cleithral or subcleithral type. No avicularia. An ancestrula was not present in the available material. Remarks Although the genus Myriapora comprises only a few species globally, owing to their mostly erect and conspicuous colonies, and because of the ubiquitous Mediterranean species M. truncata (Pallas, 1766), this bryozoan genus has received a fair amount of attention (e.g., Viskova 1986; Berning 2007; Ferretti et al . 2007; Rodolfo-Metalpa et al . 2010). Besides M. truncata and the polar M. subgracilis (d’Orbigny, 1852), M. bugei is the only other known species from the northern Atlantic realm. The most obvious difference between M. bugei and M. truncata is that in the former the branches are composed of distinct whorls whereas zooecia in the latter are ideally alternating, i.e., apparently arranged in spirals around the branch axis. The ooecia and dimorphic orifices of M. bugei are here described and figured for the first time. Originally described from the Azores, the species has also been recorded from the Great Meteor Bank (Piepenburg & Müller 2004: 61), which is located some 800 km south of the archipelago. However, although the characters are variable and overlapping to some extent, the populations from the Great Meteor Bank, as well as from the nearby Hyères and Irving seamounts, slightly differ from the type of M. bugei in having branches that predominantly consist of five zooids per whorl (occasionally four or six), smaller autozooids, and a narrower autozooecial sinus (pers. observation). Thus, especially considering the distance between the Azores and the seamounts, it is likely that these populations represent distinct species, although genetic studies may be needed to clarify this issue. In the Azores, M . bugei was reported from depths between 190 and 1235 m (d’Hondt 1975). It occurs on rocky, gravelly, sandy and muddy substrata growing on rocks, dead corals and bivalve shells. The specimens El Hajjaji (1992) described and figured as M. bugei from the Late Miocene of NE Morocco (Mediterranean Sea) are similar to the type but certainly belong to a different species due to a distinctly narrower sinus and larger condyles. The status of other coeval specimens from NW Morocco (Atlantic) cannot be assessed, as a detailed description or figures were not provided by Sefian et al . (1999: 242). : Published as part of Berning, Björn, 2013, New and little-known Cheilostomata (Bryozoa, Gymnolaemata) from the NE Atlantic, pp. 1-25 in European Journal of Taxonomy 44 on pages 13-16, DOI: 10.5852/ejt.2013.44, http://zenodo.org/record/3814003 : {"references": ["d'Hondt J. - L. 1975. Bryozoaires Ctenostomes et Cheilostomes (Cribrimorphes et Escharellidae exceptes) provenant des dragages de la campagne oceanographique Biacores du \" Jean Charcot \". Bulletin du Museum National d'Histoire Naturelle, Paris, 3 e serie 299: 553 - 600.", "El Hajjaji K. 1992. Les Bryozoaires du Miocene superieur du Maroc nord-oriental. Documents des Laboratoires de Geologie Lyon 123: 1 - 355.", "Tricart S. & d'Hondt J. - L. 2009. Catalogue des specimens-types de Bryozoaires, Brachiopodes, Pterobranches et Enteropneustes du Departement \" Milieux et Peuplements Aquatiques \" (Museum National d'Histoire Naturelle, Paris). Memoires de la Societe Linneenne de Bordeaux 11: 1 - 144.", "Viskova L. A. 1986. The morphology and colonial integration of the genus Myriapora (Cheilostomata). Paleontologicheskii Zhurnal 4: 56 - 64.", "Berning B. 2007. The Mediterranean bryozoan Myriapora truncata (Pallas, 1766): a potential indicator of (palaeo-) environmental conditions. Lethaia 40: 221 - 232. http: // dx. doi. org / 10.1111 / j. 1502 - 3931.2007.00019. x", "Ferretti C., Magnino G. & Balduzzi A. 2007. Morphology of the larva and ancestrula of Myriapora truncata (Bryozoa, Cheilostomatida). Italian Journal of Zoology 74: 341 - 350. http: // dx. doi. org / 10.1080 / 11250000701629572", "Rodolfo-Metalpa R., Lombardi C., Cocito S., Hall-Spencer J. M. & Gambi M. C. 2010. Effects of ocean acidification and high temperatures on the bryozoan Myriapora truncata at natural CO 2 vents. Marine Ecology 31: 447 - 456. http: // dx. doi. org / 10.1111 / j. 1439 - 0485.2009.00354. x", "Piepenburg D. & Muller B. 2004. Distribution of epibenthic communities on the Great Meteor Seamount (north-east Atlantic) mirrors pelagic processes. Archive of Fishery and Marine Research 51: 55 - 70.", "Sefian N. L., Pouyet S. & El Hajjaji K. 1999. Bryozoaires du Miocene superieur de Charf el Akab (NW Maroc). Revue de Paleobiologie 18: 221 - 252."]} |
format |
Text |
author |
Berning, Björn |
author_facet |
Berning, Björn |
author_sort |
Berning, Björn |
title |
Myriapora bugei d'Hondt 1975 |
title_short |
Myriapora bugei d'Hondt 1975 |
title_full |
Myriapora bugei d'Hondt 1975 |
title_fullStr |
Myriapora bugei d'Hondt 1975 |
title_full_unstemmed |
Myriapora bugei d'Hondt 1975 |
title_sort |
myriapora bugei d'hondt 1975 |
publisher |
Zenodo |
publishDate |
2013 |
url |
https://dx.doi.org/10.5281/zenodo.3815230 https://zenodo.org/record/3815230 |
long_lat |
ENVELOPE(139.017,139.017,-69.367,-69.367) ENVELOPE(8.500,8.500,-48.000,-48.000) ENVELOPE(8.500,8.500,-48.000,-48.000) |
geographic |
Charcot Meteor Bank Meteor Seamount |
geographic_facet |
Charcot Meteor Bank Meteor Seamount |
genre |
North East Atlantic Ocean acidification |
genre_facet |
North East Atlantic Ocean acidification |
op_relation |
http://zenodo.org/record/3814003 http://publication.plazi.org/id/CE7CFF90FF8AD8358818FFF3FFC94B01 http://zoobank.org/F7FD3319-AD9D-4DBB-9755-C541759C0D66 https://zenodo.org/communities/biosyslit https://dx.doi.org/10.5852/ejt.2013.44 http://zenodo.org/record/3814003 http://publication.plazi.org/id/CE7CFF90FF8AD8358818FFF3FFC94B01 https://dx.doi.org/10.5281/zenodo.3814011 http://zoobank.org/F7FD3319-AD9D-4DBB-9755-C541759C0D66 https://dx.doi.org/10.5281/zenodo.3815229 https://zenodo.org/communities/biosyslit |
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Open Access Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC0 |
op_doi |
https://doi.org/10.5281/zenodo.3815230 https://doi.org/10.5852/ejt.2013.44 https://doi.org/10.5281/zenodo.3814011 https://doi.org/10.5281/zenodo.3815229 |
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ftdatacite:10.5281/zenodo.3815230 2023-05-15T17:38:59+02:00 Myriapora bugei d'Hondt 1975 Berning, Björn 2013 https://dx.doi.org/10.5281/zenodo.3815230 https://zenodo.org/record/3815230 unknown Zenodo http://zenodo.org/record/3814003 http://publication.plazi.org/id/CE7CFF90FF8AD8358818FFF3FFC94B01 http://zoobank.org/F7FD3319-AD9D-4DBB-9755-C541759C0D66 https://zenodo.org/communities/biosyslit https://dx.doi.org/10.5852/ejt.2013.44 http://zenodo.org/record/3814003 http://publication.plazi.org/id/CE7CFF90FF8AD8358818FFF3FFC94B01 https://dx.doi.org/10.5281/zenodo.3814011 http://zoobank.org/F7FD3319-AD9D-4DBB-9755-C541759C0D66 https://dx.doi.org/10.5281/zenodo.3815229 https://zenodo.org/communities/biosyslit Open Access Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 info:eu-repo/semantics/openAccess CC0 Biodiversity Taxonomy Animalia Bryozoa Gymnolaemata Cheilostomatida Myriaporidae Myriapora Myriapora bugei Text Taxonomic treatment article-journal ScholarlyArticle 2013 ftdatacite https://doi.org/10.5281/zenodo.3815230 https://doi.org/10.5852/ejt.2013.44 https://doi.org/10.5281/zenodo.3814011 https://doi.org/10.5281/zenodo.3815229 2021-11-05T12:55:41Z Myriapora bugei d’Hondt, 1975 Fig. 4, Table 4 Myriapora bugei d’Hondt, 1975: 585, figs 23, 25-28. non Myriapora bugei – El Hajjaji 1992: 250, pl. 15, figs 14-15. Material examined Lectotype (here designated) MNHN IB-2013-3, one dried colony fragment (former part of MNHN 7481), Jean Charcot , Biaçores Stn 109, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17’ W, 190–230 m. Paralectotypes (here designated) MNHN 7481, Jean Charcot , Biaçores Stn 109, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17’ W, 190–230 m; MNHN IB- 2013-2, one dried colony fragment (former part of MNHN 7492), Jean Charcot , Biaçores Stn 110, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17.5’ W, 300–350 m; MNHN 7482, 13 colony fragments in ethanol, Jean Charcot , Biaçores Stn 109, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17’ W, 190–230 m; MNHN 7488, one colony fragment in ethanol, Jean Charcot , Biaçores Stn 110, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17.5’ W, 300–350 m; MNHN 7492, four colony fragments in ethanol, Jean Charcot , Biaçores Stn 110, 20 Oct. 1971, NW of Flores (Azores), 39°33’ N – 31°17.5’ W, 300– 350 m. The original material available to d’Hondt (1975: 560) was from Biaçores stations 109 and 110. However, he did not indicate type material when introducing Myriapora bugei , and the figured specimen (figs 23, 25-28) was subsequently destroyed (J.-L. d’Hondt pers. comm. 2012). For the same reasons as stated in the Material section for Cellaria harmelini (see above), the type specimens of M. bugei were invalidly considered as “ holotype ” and “ paratypes ” by Tricart & d’Hondt (2009), and are formally designated here as lectotype and paralectotypes, respectively. Description Colony erect, rigid, delicate branching, producing lateral offsets at an angle of about 90° at irregular intervals (Fig. 4A). Branches long (3-4 cm), slender and cylindrical, with the zooids opening all around. Zooids large, radially arranged in distinct whorls of 4 (rarely 5), with all orifices at same level and the distal whorl ideally alternating (Fig. 4 B-C); zooecia elongate rectangular but boundaries invisible on colony surface. Frontal shield of mature zooecia gently raising towards orifice, giving distal branches an undulating morphology that is slightly reduced due to frontal calcification during ontogeny (Fig. 4 A- C); frontal shield regularly perforated by numerous elongate pores in spindle-shaped depressions that are longitudinally aligned (Fig. 4B), surface finely granular (Fig. 4 D-E). Primary orifice dimorphic; in autozooids slightly longer than wide (Fig. 4D), anter horseshoe-shaped, widest slightly distal to middistance, proximolateral corners rounded with the short shoulders slightly sloping towards a deep and broadly U-shaped sinus occupying about two-thirds of total proximal width, condyles conspicuous, broad and with rounded edges, not extending beyond shoulders of the proximolateral margin; orifice in ovicellate zooids D-shaped (Fig. 4E), of similar length as in autozooids but especially the proximal margin distinctly broader, sinus a very shallow straight edge comprising four-fifths of total proximal width, proximolateral shoulders thus relatively short and fairly straight, condyles similar to those in autozooids; orifice becoming immersed by frontal calcification and occasionally closed during ontogeny in proximal branch regions, in which case a small short peristome with a central pore remains. No oral spines. Ovicells relatively rare, present in all zooids of certain whorls, indicated by a slightly thicker swelling of this branch region and by frontal pseudopores that are radially arranged from the proximal ooecium centre (Fig. 4B, E), ooecium mostly incorporated into frontal shields of the distal zooids, surface as frontal shield of zooecia, boundaries invisible at colony surface, ovicell aperture at an acute angle to frontal plane, closure of the cleithral or subcleithral type. No avicularia. An ancestrula was not present in the available material. Remarks Although the genus Myriapora comprises only a few species globally, owing to their mostly erect and conspicuous colonies, and because of the ubiquitous Mediterranean species M. truncata (Pallas, 1766), this bryozoan genus has received a fair amount of attention (e.g., Viskova 1986; Berning 2007; Ferretti et al . 2007; Rodolfo-Metalpa et al . 2010). Besides M. truncata and the polar M. subgracilis (d’Orbigny, 1852), M. bugei is the only other known species from the northern Atlantic realm. The most obvious difference between M. bugei and M. truncata is that in the former the branches are composed of distinct whorls whereas zooecia in the latter are ideally alternating, i.e., apparently arranged in spirals around the branch axis. The ooecia and dimorphic orifices of M. bugei are here described and figured for the first time. Originally described from the Azores, the species has also been recorded from the Great Meteor Bank (Piepenburg & Müller 2004: 61), which is located some 800 km south of the archipelago. However, although the characters are variable and overlapping to some extent, the populations from the Great Meteor Bank, as well as from the nearby Hyères and Irving seamounts, slightly differ from the type of M. bugei in having branches that predominantly consist of five zooids per whorl (occasionally four or six), smaller autozooids, and a narrower autozooecial sinus (pers. observation). Thus, especially considering the distance between the Azores and the seamounts, it is likely that these populations represent distinct species, although genetic studies may be needed to clarify this issue. In the Azores, M . bugei was reported from depths between 190 and 1235 m (d’Hondt 1975). It occurs on rocky, gravelly, sandy and muddy substrata growing on rocks, dead corals and bivalve shells. The specimens El Hajjaji (1992) described and figured as M. bugei from the Late Miocene of NE Morocco (Mediterranean Sea) are similar to the type but certainly belong to a different species due to a distinctly narrower sinus and larger condyles. The status of other coeval specimens from NW Morocco (Atlantic) cannot be assessed, as a detailed description or figures were not provided by Sefian et al . (1999: 242). : Published as part of Berning, Björn, 2013, New and little-known Cheilostomata (Bryozoa, Gymnolaemata) from the NE Atlantic, pp. 1-25 in European Journal of Taxonomy 44 on pages 13-16, DOI: 10.5852/ejt.2013.44, http://zenodo.org/record/3814003 : {"references": ["d'Hondt J. - L. 1975. Bryozoaires Ctenostomes et Cheilostomes (Cribrimorphes et Escharellidae exceptes) provenant des dragages de la campagne oceanographique Biacores du \" Jean Charcot \". Bulletin du Museum National d'Histoire Naturelle, Paris, 3 e serie 299: 553 - 600.", "El Hajjaji K. 1992. Les Bryozoaires du Miocene superieur du Maroc nord-oriental. Documents des Laboratoires de Geologie Lyon 123: 1 - 355.", "Tricart S. & d'Hondt J. - L. 2009. Catalogue des specimens-types de Bryozoaires, Brachiopodes, Pterobranches et Enteropneustes du Departement \" Milieux et Peuplements Aquatiques \" (Museum National d'Histoire Naturelle, Paris). Memoires de la Societe Linneenne de Bordeaux 11: 1 - 144.", "Viskova L. A. 1986. The morphology and colonial integration of the genus Myriapora (Cheilostomata). Paleontologicheskii Zhurnal 4: 56 - 64.", "Berning B. 2007. The Mediterranean bryozoan Myriapora truncata (Pallas, 1766): a potential indicator of (palaeo-) environmental conditions. Lethaia 40: 221 - 232. http: // dx. doi. org / 10.1111 / j. 1502 - 3931.2007.00019. x", "Ferretti C., Magnino G. & Balduzzi A. 2007. Morphology of the larva and ancestrula of Myriapora truncata (Bryozoa, Cheilostomatida). Italian Journal of Zoology 74: 341 - 350. http: // dx. doi. org / 10.1080 / 11250000701629572", "Rodolfo-Metalpa R., Lombardi C., Cocito S., Hall-Spencer J. M. & Gambi M. C. 2010. Effects of ocean acidification and high temperatures on the bryozoan Myriapora truncata at natural CO 2 vents. Marine Ecology 31: 447 - 456. http: // dx. doi. org / 10.1111 / j. 1439 - 0485.2009.00354. x", "Piepenburg D. & Muller B. 2004. Distribution of epibenthic communities on the Great Meteor Seamount (north-east Atlantic) mirrors pelagic processes. Archive of Fishery and Marine Research 51: 55 - 70.", "Sefian N. L., Pouyet S. & El Hajjaji K. 1999. Bryozoaires du Miocene superieur de Charf el Akab (NW Maroc). Revue de Paleobiologie 18: 221 - 252."]} Text North East Atlantic Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Charcot ENVELOPE(139.017,139.017,-69.367,-69.367) Meteor Bank ENVELOPE(8.500,8.500,-48.000,-48.000) Meteor Seamount ENVELOPE(8.500,8.500,-48.000,-48.000) |