Pentapora clipeus Lombardi & Taylor & Cocito 2010, SP. NOV.

PENTAPORA CLIPEUS SP. NOV. (FIG. 11) Material examined: Holotype: NHM BZ 5662, Middle Pliocene, Monte Padova (level 90), Castell’Arquato, Piacenza, Emilia, Italy, Pizzaferri Collection. Paratype: NHM BZ 5663, details as for holotype. Diagnosis: Pentapora with erect bifoliate colonies; autozooids sma...

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Main Authors: Lombardi, Chiara, Taylor, Paul D., Cocito, Silvia
Format: Text
Language:unknown
Published: Zenodo 2010
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.5491087
https://zenodo.org/record/5491087
id ftdatacite:10.5281/zenodo.5491087
record_format openpolar
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Biodiversity
Taxonomy
Animalia
Bryozoa
Gymnolaemata
Cheilostomatida
Bitectiporidae
Pentapora
Pentapora clipeus
spellingShingle Biodiversity
Taxonomy
Animalia
Bryozoa
Gymnolaemata
Cheilostomatida
Bitectiporidae
Pentapora
Pentapora clipeus
Lombardi, Chiara
Taylor, Paul D.
Cocito, Silvia
Pentapora clipeus Lombardi & Taylor & Cocito 2010, SP. NOV.
topic_facet Biodiversity
Taxonomy
Animalia
Bryozoa
Gymnolaemata
Cheilostomatida
Bitectiporidae
Pentapora
Pentapora clipeus
description PENTAPORA CLIPEUS SP. NOV. (FIG. 11) Material examined: Holotype: NHM BZ 5662, Middle Pliocene, Monte Padova (level 90), Castell’Arquato, Piacenza, Emilia, Italy, Pizzaferri Collection. Paratype: NHM BZ 5663, details as for holotype. Diagnosis: Pentapora with erect bifoliate colonies; autozooids small, averaging 0.55-mm long by 0.37-mm wide; giant avicularia spatulate, often with closure plate containing two pores, crossbar uncalcified; ovicell with pores in a band close to orifice. Description: Colonies erect, bilamellar, represented only by small fragments. Base and early astogeny unknown. Autozooids small, longer than wide, 0.48–0.60 mm long (mean 0.55 ± 0.06 mm; N = 5), 0.33–0.42 mm wide (mean 0.37 ± 0.04 mm; N = 5). Frontal shield lepralioid, slightly convex, granular, with areolar pores and pseudopores; zooidal boundaries becoming less distinct during ontogeny. Primary orifice slightly longer than wide, 0.18–0.25 mm long (mean 0.22 ± 0.03 mm; N = 5), 0.17–0.22 mm wide (mean 0.20 ± 0.02 mm; N = 5); condyles present; lappets sometimes developed. Oral spines often present but few in number. Basal walls with short median septum extending distally from transverse wall. Ovicells globular, becoming completely embedded by calcification of the frontal shield of the distal zooid; pores present in a band close to the primary orifice. Avicularia dimorphic, adventitious, suboral, proximally directed. Normal avicularia small, 0.07– 0.08 mm long (mean 0.080 ± 0.005 mm; N = 5), 0.06– 0.07 mm wide (mean 0.070 ± 0.006 mm; N = 5). Giant avicularia often substituting for normal avicularia, 0.17–0.27 mm long (mean 0.21 ± 0.03 mm; N = 15), 0.15–0.20 mm wide (0.17 ± 0.02 mm; N = 15), occupying less than half of the length of the autozooid, lying normal to the frontal plane partially within the primary orifice; rostrum spatulate; crossbar uncalcified; closure plates often present, containing two or occasionally three pores. Etymology: The species name (Latin, clipeus , shield) alludes to the distinctive closure plates that occlude many of the giant avicularia. Remarks: This new species is most easily recognized by the closure plates of the giant avicularia (Fig. 11A– E), structures that are not present in other species of Pentapora , except occasionally in P. lacryma sp. nov., where they lack the pores seen in P. clipeus sp. nov. The absence of a calcified crossbar in the giant avicularia is another distinctive feature (Fig. 11C): this does not seem to be simply the result of breakages, in view of the good condition of the material. Material of P. clipeus sp. nov. comes from a locality preserving aragonite, in contrast to most of the P. pertusa and P. lacryma sp. nov. specimens described above, where aragonite has been leached. This may account for the preservation of orificial lappets and secondary calcification overgrowing the ovicells (Fig. 11B). The new species shares with P. lacryma sp. nov. the possession of small autozooids. However, unlike the other fossil species of Pentapora , P. pertusa and P. lacryma sp. nov., ovicell pores are arranged in a band close to the primary orifice in P. clipeus sp. nov. (Fig. 11A, B); P. pertusa has single large ovicell pore (Fig. 8A), whereas numerous pores are scattered across the entire ovicell surface in P. lacryma sp. nov. (Fig. 9D). Distribution: Pliocene, Piacenzian, Monte Padova, Emilia, Italy. : Published as part of Lombardi, Chiara, Taylor, Paul D. & Cocito, Silvia, 2010, Systematics of the Miocene-Recent bryozoan genus Pentapora (Cheilostomata), pp. 17-39 in Zoological Journal of the Linnean Society 160 (1) on pages 31-33, DOI: 10.1111/j.1096-3642.2009.00594.x, http://zenodo.org/record/5439457 : {"references": ["Lorenz L. 1886. Bryozoen von Jan Mayen. Die Internationale Polarforschung 1882 - 83. Die Osterreichische Polarstation Jan Mayen 3: 83 - 100.", "Kuklinski P, Hayward PJ. 2004. Two new cheilostome Bryozoa from Svalbard. Sarsia 89: 79 - 84."]}
format Text
author Lombardi, Chiara
Taylor, Paul D.
Cocito, Silvia
author_facet Lombardi, Chiara
Taylor, Paul D.
Cocito, Silvia
author_sort Lombardi, Chiara
title Pentapora clipeus Lombardi & Taylor & Cocito 2010, SP. NOV.
title_short Pentapora clipeus Lombardi & Taylor & Cocito 2010, SP. NOV.
title_full Pentapora clipeus Lombardi & Taylor & Cocito 2010, SP. NOV.
title_fullStr Pentapora clipeus Lombardi & Taylor & Cocito 2010, SP. NOV.
title_full_unstemmed Pentapora clipeus Lombardi & Taylor & Cocito 2010, SP. NOV.
title_sort pentapora clipeus lombardi & taylor & cocito 2010, sp. nov.
publisher Zenodo
publishDate 2010
url https://dx.doi.org/10.5281/zenodo.5491087
https://zenodo.org/record/5491087
long_lat ENVELOPE(20.000,20.000,78.000,78.000)
ENVELOPE(167.350,167.350,-78.117,-78.117)
ENVELOPE(-57.900,-57.900,-63.300,-63.300)
geographic Svalbard
Jan Mayen
Svalbard
Hayward
Silvia
geographic_facet Svalbard
Jan Mayen
Svalbard
Hayward
Silvia
genre Jan Mayen
Svalbard
genre_facet Jan Mayen
Svalbard
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op_doi https://doi.org/10.5281/zenodo.5491087
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spelling ftdatacite:10.5281/zenodo.5491087 2023-05-15T16:57:03+02:00 Pentapora clipeus Lombardi & Taylor & Cocito 2010, SP. NOV. Lombardi, Chiara Taylor, Paul D. Cocito, Silvia 2010 https://dx.doi.org/10.5281/zenodo.5491087 https://zenodo.org/record/5491087 unknown Zenodo http://zenodo.org/record/5439457 http://publication.plazi.org/id/FF81E40EFFF451118279FFA9FFD4F52C https://zenodo.org/communities/biosyslit https://dx.doi.org/10.1111/j.1096-3642.2009.00594.x http://zenodo.org/record/5439457 http://publication.plazi.org/id/FF81E40EFFF451118279FFA9FFD4F52C https://dx.doi.org/10.5281/zenodo.5439479 https://dx.doi.org/10.5281/zenodo.5439473 https://dx.doi.org/10.5281/zenodo.5439475 https://dx.doi.org/10.5281/zenodo.5491088 https://zenodo.org/communities/biosyslit Open Access info:eu-repo/semantics/openAccess Biodiversity Taxonomy Animalia Bryozoa Gymnolaemata Cheilostomatida Bitectiporidae Pentapora Pentapora clipeus Text Taxonomic treatment article-journal ScholarlyArticle 2010 ftdatacite https://doi.org/10.5281/zenodo.5491087 https://doi.org/10.1111/j.1096-3642.2009.00594.x https://doi.org/10.5281/zenodo.5439479 https://doi.org/10.5281/zenodo.5439473 https://doi.org/10.5281/zenodo.5439475 https://doi.org/10.5281/zenodo.5491088 2021-11-05T12:55:41Z PENTAPORA CLIPEUS SP. NOV. (FIG. 11) Material examined: Holotype: NHM BZ 5662, Middle Pliocene, Monte Padova (level 90), Castell’Arquato, Piacenza, Emilia, Italy, Pizzaferri Collection. Paratype: NHM BZ 5663, details as for holotype. Diagnosis: Pentapora with erect bifoliate colonies; autozooids small, averaging 0.55-mm long by 0.37-mm wide; giant avicularia spatulate, often with closure plate containing two pores, crossbar uncalcified; ovicell with pores in a band close to orifice. Description: Colonies erect, bilamellar, represented only by small fragments. Base and early astogeny unknown. Autozooids small, longer than wide, 0.48–0.60 mm long (mean 0.55 ± 0.06 mm; N = 5), 0.33–0.42 mm wide (mean 0.37 ± 0.04 mm; N = 5). Frontal shield lepralioid, slightly convex, granular, with areolar pores and pseudopores; zooidal boundaries becoming less distinct during ontogeny. Primary orifice slightly longer than wide, 0.18–0.25 mm long (mean 0.22 ± 0.03 mm; N = 5), 0.17–0.22 mm wide (mean 0.20 ± 0.02 mm; N = 5); condyles present; lappets sometimes developed. Oral spines often present but few in number. Basal walls with short median septum extending distally from transverse wall. Ovicells globular, becoming completely embedded by calcification of the frontal shield of the distal zooid; pores present in a band close to the primary orifice. Avicularia dimorphic, adventitious, suboral, proximally directed. Normal avicularia small, 0.07– 0.08 mm long (mean 0.080 ± 0.005 mm; N = 5), 0.06– 0.07 mm wide (mean 0.070 ± 0.006 mm; N = 5). Giant avicularia often substituting for normal avicularia, 0.17–0.27 mm long (mean 0.21 ± 0.03 mm; N = 15), 0.15–0.20 mm wide (0.17 ± 0.02 mm; N = 15), occupying less than half of the length of the autozooid, lying normal to the frontal plane partially within the primary orifice; rostrum spatulate; crossbar uncalcified; closure plates often present, containing two or occasionally three pores. Etymology: The species name (Latin, clipeus , shield) alludes to the distinctive closure plates that occlude many of the giant avicularia. Remarks: This new species is most easily recognized by the closure plates of the giant avicularia (Fig. 11A– E), structures that are not present in other species of Pentapora , except occasionally in P. lacryma sp. nov., where they lack the pores seen in P. clipeus sp. nov. The absence of a calcified crossbar in the giant avicularia is another distinctive feature (Fig. 11C): this does not seem to be simply the result of breakages, in view of the good condition of the material. Material of P. clipeus sp. nov. comes from a locality preserving aragonite, in contrast to most of the P. pertusa and P. lacryma sp. nov. specimens described above, where aragonite has been leached. This may account for the preservation of orificial lappets and secondary calcification overgrowing the ovicells (Fig. 11B). The new species shares with P. lacryma sp. nov. the possession of small autozooids. However, unlike the other fossil species of Pentapora , P. pertusa and P. lacryma sp. nov., ovicell pores are arranged in a band close to the primary orifice in P. clipeus sp. nov. (Fig. 11A, B); P. pertusa has single large ovicell pore (Fig. 8A), whereas numerous pores are scattered across the entire ovicell surface in P. lacryma sp. nov. (Fig. 9D). Distribution: Pliocene, Piacenzian, Monte Padova, Emilia, Italy. : Published as part of Lombardi, Chiara, Taylor, Paul D. & Cocito, Silvia, 2010, Systematics of the Miocene-Recent bryozoan genus Pentapora (Cheilostomata), pp. 17-39 in Zoological Journal of the Linnean Society 160 (1) on pages 31-33, DOI: 10.1111/j.1096-3642.2009.00594.x, http://zenodo.org/record/5439457 : {"references": ["Lorenz L. 1886. Bryozoen von Jan Mayen. Die Internationale Polarforschung 1882 - 83. Die Osterreichische Polarstation Jan Mayen 3: 83 - 100.", "Kuklinski P, Hayward PJ. 2004. Two new cheilostome Bryozoa from Svalbard. Sarsia 89: 79 - 84."]} Text Jan Mayen Svalbard DataCite Metadata Store (German National Library of Science and Technology) Svalbard Jan Mayen Svalbard ENVELOPE(20.000,20.000,78.000,78.000) Hayward ENVELOPE(167.350,167.350,-78.117,-78.117) Silvia ENVELOPE(-57.900,-57.900,-63.300,-63.300)