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Journal articles on the topic 'Bioclaustration'

Author: Grafiati
Published: 4 June 2025
Last updated: 1 August 2025

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1

VINN, OLEV, MARK A. WILSON, MARE ISAKAR, and URSULA TOOM. "NEW BIOCLAUSTRATION OF A SYMBIONT IN THE MANTLE CAVITY OF CLITAMBONITES SCHMIDTI (BRACHIOPODA) FROM THE SANDBIAN (UPPER ORDOVICIAN) OF ESTONIA." PALAIOS 37, no. 9 (2022): 520–24. http://dx.doi.org/10.2110/palo.2021.067.

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Abstract A new bioclaustration of a symbiont is here described from the mantle cavity of the strophomenatan brachiopod Clitambonites schmidti. It is the second bioclaustration in brachiopods known from the Kukruse Regional Stage (Sandbian) of Estonia. It shares affinities with the bioclaustrations Burrinjuckia and Haplorygma. The outgrowth in the ventral valve interior was secreted by the brachiopod around a symbiont. Most likely the symbiont was a suspension feeder that collected food particles from the brachiopod's mantle cavity. The symbiont was either a kleptoparasite or fed on the brachio
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2

Vinn, Olev, Abdullah A. Alkahtane, Saleh Al Farraj, and Magdy El Hedeny. "First record of Chaetosalpinx bioclaustrations in the rugose corals from the Late Ordovician of Baltica." Revista Brasileira de Paleontologia 27, no. 4 (2025): e20240475. https://doi.org/10.4072/rbp.2024.4.0475.

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Bioclaustrations are extremely rare in the rugose corals from the Ordovician of Estonia. A specimen of Kenophyllum subcylindricum from the Vormsi Regional Stage (Katian) contains multiple shafts of Chaetosalpinx siberiensis?. The latter bioclaustration also occurs in the Pirgu Regional Stage (Katian). The growth lines of the host coral show a reaction to the infesting organism, suggesting that the shafts in the calyx are bioclaustrations and not post-mortem borings (Trypanites). The worm-like Chaetosalpinx tracemaker initially caused damage to the coral’s soft tissues and used the coral’s reso
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3

Tapanila, Leif. "Direct Evidence of Ancient Symbiosis Using Trace Fossils." Paleontological Society Papers 14 (October 2008): 271–87. http://dx.doi.org/10.1017/s1089332600001728.

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Symbiotic associations are a poorly studied aspect of the fossil record, owing largely to the taphonomic biases that inhibit direct observation that two organisms shared an intimate association in life. A symbiosis between an infesting animal and a skeleton-producing host can form a bioclaustration cavity that directly preserves the association and has a high preservation potential. Identification of ancient mutuals and parasites must reject the null hypothesis of commensalism by demonstrating that the symbiosis correlates with a positive or negative change in host fitness as compared to a non
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4

Ernst, Andrej, Paul D. Taylor, and Jan Bohatý. "A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration." Acta Palaeontologica Polonica 59, no. 1 (2012): 173–83. https://doi.org/10.4202/app.2010.0110.

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Ernst, Andrej, Taylor, Paul D., Bohatý, Jan (2014): A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration. Acta Palaeontologica Polonica 59 (1): 173-183, DOI: 10.4202/app.2010.0110, URL: http://dx.doi.org/10.4202/app.2010.0110
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5

Suárez Andrés, Juan L. "Bioclaustration in Devonian fenestrate bryozoans. The ichnogenus Caupokeras McKinney, 2009." Spanish Journal of Palaeontology 29, no. 1 (2020): 5. http://dx.doi.org/10.7203/sjp.29.1.17483.

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6

Zhang, Yuchen, Xiaocong Luan, Renbin Zhan, Colin D. Sproat, and Bing Huang. "Early parasitic drilling in a rhynchonelliform brachiopod Rongatrypa xichuanensis from the Katian (Upper Ordovician) of central China." Journal of Paleontology 94, no. 3 (2020): 467–74. http://dx.doi.org/10.1017/jpa.2019.102.

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AbstractAn example of parasitic drilling in a rhynchonelliform brachiopod is described from the Shiyanhe Formation (Katian, Upper Ordovician) of Henan, central China. The boring extends into the shell almost perpendicular to the surface. The shell has been serially sectioned, and the trace (including boring and bioclaustration) has been modeled in three dimensions. Healing of the shell evident in serial sections supports a long-term relationship between the brachiopod and borer that we interpret as parasitic. Platyceratid gastropods, found at the same locality as these brachiopods, are the mos
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7

Cónsole-Gonella, Carlos, and Rosa A. Marquillas. "Bioclaustration trace fossils in epeiric shallow marine stromatolites: the Cretaceous-Palaeogene Yacoraite Formation, Northwestern Argentina." Lethaia 47, no. 1 (2013): 107–19. http://dx.doi.org/10.1111/let.12043.

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8

Richiano, Sebastián, Marina Aguirre, Ester Farinati, Karen Davies, Ignacio Castellanos, and Lucia E. Gómez-Peral. "Enigmatic traces in infaunal bivalves from the late Quaternary of Argentina, Southwestern Atlantic. Bioerosion, bioclaustration or nothing?" Geobios 51, no. 2 (2018): 161–72. http://dx.doi.org/10.1016/j.geobios.2018.02.003.

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9

Cruz-Guevara, Luis Enrique, Luis Felipe Cruz-Ceballos, and Gladys Marcela Avendaño-Sanchez. "Biogenic production and their sedimentary record: a review." Boletín de Ciencias de la Tierra, no. 55 (February 1, 2024): 11–24. http://dx.doi.org/10.15446/rbct.n55.110363.

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The recognized biogenic production corresponds to corporal materials, and ethological structures (ichnofossils). Ethological structures include bioturbation, bioerosion, and biogenic granule-classification structures. Biogenic materials and structures traditionally include biogenic aggregates (such as fecal pellets or castings and coprolite grapstones); bioturbation structures or ichno-structures (burrows, tracks, trails, and root penetration structures); biogenic granulo-classification or biostratification structures (algal and bacterial stromatolites of graded bedding of biogenic origin); bi
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10

Słowiński, Jakub, Dawid Surmik, Piotr Duda, and Michał Zatoń. "Assessment of serpulid-hydroid association through the Jurassic: A case study from the Polish Basin." PLOS ONE 15, no. 12 (2020): e0242924. http://dx.doi.org/10.1371/journal.pone.0242924.

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The coexistence of sessile, tube-dwelling polychaetes (serpulids) and hydroids, has been investigated. Serpulid tubes bearing traces after hydroids are derived from different stratigraphic intervals spanning the Middle and Upper Jurassic, the rocks of which represent the diverse paleoenvironments of the Polish Basin. Although fossil colonial hydroids classified under the species Protulophila gestroi are a commonly occurring symbiont of these polychaetes during the Late Cretaceous and Cenozoic, they seem to be significantly less frequent during the Jurassic and limited to specific paleoenvironm
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11

Vinn, Olev, Andrej Ernst, and Ursula Toom. "Bioclaustrations in Upper Ordovician bryozoans from northern Estonia." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 289, no. 1 (2018): 113–21. http://dx.doi.org/10.1127/njgpa/2018/0752.

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12

Tovar-Hernández, María Ana, María Elena García-Garza, and León-González Jesús Angel de. "Sclerozoan and fouling sabellid worms (Annelida: Sabellidae) from Mexico with the establishment of two new species." Biodiversity Data Journal 8 (October 8, 2020): e57471. https://doi.org/10.3897/BDJ.8.e57471.

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The sabellid genera <em>Anamobaea</em> Krøyer, 1856 and <em>Notaulax </em>Tauber, 1879 are two of the most attractive polychaete worms in coral reefs. <em>Anamobaea</em> is represented by two Caribbean species and <em>Notaulax</em> with 24 species from around the world, six of them previously known to tropical America. During examination of fouling biota and sclerozoans from Mexico, <em>Anamobaea orstedii</em> Krøyer, 1856 was found in coral reefs from the southern Gulf of Mexico and three species of <em>Notaulax</em> were identified to the Mexican Pacific, two of them being new species to sci
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13

Tapanila, Leif. "Macroborings and Bioclaustrations in a Late Devonian Reef Above the Alamo Impact Breccia, Nevada, USA." Ichnos 13, no. 3 (2006): 129–34. http://dx.doi.org/10.1080/10420940600850893.

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14

Wilson, Mark A., Olev Vinn, and Timothy J. Palmer. "Bivalve borings, bioclaustrations and symbiosis in corals from the Upper Cretaceous (Cenomanian) of southern Israel." Palaeogeography, Palaeoclimatology, Palaeoecology 414 (November 2014): 243–45. http://dx.doi.org/10.1016/j.palaeo.2014.09.005.

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15

Vinn, Olev, Andrej Ernst, Mark A. Wilson, and Ursula Toom. "Borings and bioclaustrations in bryozoans from the Kunda Regional Stage (Darriwilian; Middle Ordovician) of northern Estonia and NW Russia." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 303, no. 2 (2022): 219–25. http://dx.doi.org/10.1127/njgpa/2022/1044.

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16

Buttler, Caroline J., and Mark A. Wilson. "Paleoecology of an Upper Ordovician submarine cave-dwelling bryozoan fauna and its exposed equivalents in northern Kentucky, USA." Journal of Paleontology 92, no. 4 (2018): 568–76. http://dx.doi.org/10.1017/jpa.2017.131.

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AbstractA bryozoan-dominated fauna that inhabited small caves underneath a carbonate hardground is here described from the Corryville Formation (Upper Ordovician, Katian) exposed near Washington, Mason County, Kentucky, USA. The dominant bryozoan,Stigmatella personata(a trepostome), is found both growing downwards from the cave ceilings and upwards on the exposed hardground surface above. Another trepostome,Monticulipora, is a minor component of the cave fauna. There are few discernible anatomical differences between the bryozoan colonies that grew upwards in presumably well-lit waters and tho
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17

Vinn, Olev, Mark A. Wilson, Andrej Ernst, and Ursula Toom. "The Ordovician bioclaustration revolution." Geobios, May 2023. http://dx.doi.org/10.1016/j.geobios.2022.10.007.

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18

Ernst, Andrej. "A new Middle Devonian cystoporate bryozoan from Germany containing a new symbiont bioclaustration." Acta Palaeontologica Polonica, 2012. http://dx.doi.org/10.4202/app.2010.0110.

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19

Thomka, James, and Lilian Gunderson. "Multiple forms of bioimmuration in a coral-crinoid-bryozoan association from the Middle Devonian Onondaga Formation of southeastern Ontario." Canadian Journal of Earth Sciences, June 1, 2023. http://dx.doi.org/10.1139/cjes-2023-0002.

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A large favositid tabulate coral colony from the Middle Devonian Edgecliff Member of the Onondaga Formation, collected from Port Colborne, southernmost Ontario, is described herein because of several noteworthy paleontological features preserved via overgrowth by the coral. The initial substratum colonized and subsequently overgrown by the favositid was a large solitary rugose coral; and outward growth resulted in overgrowth of multiple macrofossils, including relatively long portions of large-diameter (probably camerate) crinoid columns. The crinoid columns, which likely represent portions of
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20

Wisshak, Max, Simon Schneider, Radek Mikuláš, Sebastián Richiano, Fran Ramil, and Mark A. Wilson. "Putative hydroid symbionts recorded by bioclaustrations in fossil molluscan shells: a revision and reinterpretation of the cecidogenus Rodocanalis." Papers in Palaeontology 9, no. 2 (2023). http://dx.doi.org/10.1002/spp2.1484.

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