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Relevant bibliographies by topics / Bioclaustration

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Journal articles

Academic literature on the topic 'Bioclaustration'

Author: Grafiati

Published: 4 June 2025

Last updated: 1 August 2025

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Journal articles on the topic "Bioclaustration"

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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