Genus
Trypanites Mägdefrau, 1932
Taxon description
Wisshak et al., 2019a
Macroboring; substrate calcareous; tracemaker invertebrate
Knaust et al., 2023a
Diagnosis. Single-entrance, cylindrical, unbranched borings in hard substrates, having a circular cross-section throughout length. The axes of the borings may be straight, curved or irregular (after Bromley & D’Alessandro 1987; modified by Neumann et al. 2008).
Buatois et al., 2017
Category of architectural design: 2.59. Cylindrical vertical to oblique borings.
Knaust, 2012a
Unbranched, cylindrical
Bhattacharaya & Banerjee, 2014
Diagnosis.—Included in Trypanites are simple unbranched vertical to sinuous borings with a single opening to the surface; with or without a flared entrance. Circular in cross section; generally isodiametric throughout the entire length but may terminate in a small cupulate chamber.
Blissett & Pickerill, 2007
Diagnosis– (Modified after Bromley & D’Alessandro, 1987, p. 403.) Single entrance, cylindrical or sub-cylindrical, unbranched boring in lithic or biogenic substrates having circular cross-section throughout length. The axes of the boring may be straight, curved or irregular.
Taylor & Wilson, 2003
Remark: Cylindrical, unbranched boring; length up to 50 times width. Some Ordovician examples described by Kobluk and Nemcsok (1982) contain scolecodonts suggesting that the borings were made by polychaete worms.
Selection of related publications
Knaust, D., Dronov, A. V., Toom, U. 2023. Two almost‐forgotten Trypanites ichnospecies names for the most common Palaeozoic macroboring. Papers in Palaeontology 9, 3, e1491. DOI:10.1002/spp2.1491
Toom, U., Kuva, J., Knaust, D. 2023. Ichnogenus Trypanites in the Ordovician of Estonia (Baltica). Estonian Journal of Earth Sciences 72, 1, 106-109. DOI:10.3176/earth.2023.48
Toom, U., Kröger, B., Knaust, D. 2023. A Balanoglossites-Trypanites ichnofabric from the Upper Ordovician warm-water carbonates of Estonia.Following in the footsteps of Richard Granville Bromley. Abstracts and Field Guide , pp. 38-38.
Knaust, D., Dronov, A., Toom, U. 2023. Two almost forgotten Trypanites ichnospecies names for the most common Palaeozoic macroboring.Bio-i geosobytiâ v istorii Zemli. Ètapnost' èvolûcii i stratigrafičeskaâ korrelâciâ. LXIX sessiâ paleontologičeskogo obŝestva , pp. 59-59. Kartafabrika VSEGEI.
Matysik, M., Stachacz, M., Knaust, D., Whitehouse, M. J. 2022. Geochemistry, ichnology, and sedimentology of omission levels in Middle Triassic (Muschelkalk) platform carbonates of the Germanic Basin (southern Poland). Palaeogeography, Palaeoclimatology, Palaeoecology 585, 110732. DOI:10.1016/j.palaeo.2021.110732
Toom, U., Vinn, O., Hints, O. 2019. Ordovician and Silurian ichnofossils from carbonate facies in Estonia: A collection-based review. Palaeoworld 28, 1-2, 123-144. DOI:10.1016/j.palwor.2018.07.001
Vinn, O., Toom, U. 2016. Borings in phosphatized Cambrian siltstone pebbles, Estonia (Baltica). Geological Magazine 153, 4, 635-642. DOI:10.1017/S001675681500076X
Vinn, O., Toom, U. 2016. Bioerosion of inorganic hard substrates in the Silurian of Estonia (Baltica). GFF 138, 2, 306-310. DOI:10.1080/11035897.2015.1076513
Vinn, O., Toom, U. 2016. A sparsely encrusted hardground with abundant Trypanites borings from the Llandovery of the Velise River, western Estonia (Baltica). Estonian Journal of Earth Sciences 65, 1, 19-26. DOI:10.3176/earth.2016.01
Vinn, O., Wilson, M. A., Toom, U. 2015. Bioerosion of Inorganic Hard Substrates in the Ordovician of Estonia (Baltica). PLOS ONE 10, 7, e0134279. DOI:10.1371/journal.pone.0134279
Vinn, O., Wilson, M. A. 2012. Encrustation and bioerosion on late Sheinwoodian (Wenlock, Silurian) stromatoporoids from Saaremaa, Estonia. Carnets de Géologie 12, 2, 183-191. DOI:10.4267/2042/47551
Vinn, O., Wilson, M. A. 2010. Occurrence of Giant Borings of Osprioneides kampto in the Lower Silurian (Sheinwoodian) Stromatoporoids of Saaremaa, Estonia. Ichnos 17, 3, 166-171. DOI:10.1080/10420940.2010.502478
Vinn, O., Wilson, M. A. 2010. Early large borings in a hardground of Floian-Dapingian age (Early and Middle Ordovician) in northeastern Estonia (Baltica). Carnets de Géologie 10, le, 1-4. DOI:10.4267/2042/35594
Neumann, C., Wisshak, M., Bromley, R. G. 2008. Boring a mobile domicile: an alternative to the conchicolous life habit.Current Developments in Bioerosion , pp. 307-327. Springer. DOI:10.1007/978-3-540-77598-0_16
Wyse Jackson, P. N., Key, M. M. 2007. Borings in trepostome bryozoans from the Ordovician of Estonia: two ichnogenera produced by a single maker, a case of host morphology control. Lethaia 40, 3, 237-252. Wiley. DOI:10.1111/j.1502-3931.2007.00021.x
Vinn, O. 2005. The tube ultrastructure of serpulids (Annelida, Polychahaeta) Pentaditrypa subtorquata, Cretaceous, and Nogrobs cf. vertebralis, Jurassic, from Germany. Proceedings of the Estonian Academy of Sciences. Geology 54, 4, 260-265. DOI:10.3176/geol.2005.4.03
Vinn, O. 2005. The distribution of worm borings in brachiopod shells from the Caradoc Oil Shale of Estonia. Carnets de Géologie 5, article 3, 1-11. DOI:10.4267/2042/2454
Cole, A. R., Palmer, T. J. 1999. Middle Jurassic worm borings, and a new giant ichnospecies of Trypanites from the Bajocian/Dinantian unconformity, southern England. Proceedings of the Geologists Association 110, 3, 203–209. DOI:10.1016/S0016-7878(99)80070-4
List of species
3. Trypanites keilaensis Orviku, 1940 | Lasnamägi Stage
5. Trypanites weisei Mägdefrau, 1932 | Katian
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Classification
See also
References based on distribution
- Vinn & Wilson, 2010b Undva cliff Jaani Stage
- Vinn & Wilson, 2010a Abula cliff Jaagarahu Stage
- Vinn, 2005b Lava River, Leningrad Oblast Volkhov Stage
- Vinn, 2005a Volkhov River outcrops Volkhov Stage
- Wyse Jackson & Key, 2007 Kohtla opencast Kukruse Stage
- Wyse Jackson & Key, 2007 Ristna cliff Keila Stage
- Wyse Jackson & Key, 2007 Pakri Cape Cliff Uhaku Stage
- Cole & Palmer, 1999 Torr Works Quarry, England
- Knaust et al., 2023a Gleisberg, west slope Anisian
- Neumann et al., 2008 Stevns klint, Denmark Maastrichtian
- Toom et al., 2023 Sutlema quarry Katian
- Toom et al., 2023b Äiamaa borehole Katian
- Matysik et al., 2022 Zelatowa Quarry Anisian
- Knaust et al., 2023a Keila River, upstream of the waterfall Lasnamägi Stage
- Knaust et al., 2023a Putilovo quarry, Leningrad Oblast Dapingian
- Knaust et al., 2023a Keila River, upstream of the waterfall Lasnamägi Stage
- Knaust et al., 2023a Pakri LNG terminal outcrop Darriwilian
- Knaust et al., 2023a Ohesaare cliff Ohesaare Stage
- Knaust et al., 2023a Väike-Pakri Island
- Knaust et al., 2023a Babino quarry Leningrad district
- Knaust et al., 2023b Lahepere clint
- Knaust et al., 2023a Syass River, outcrop 9 Volkhov Stage
- Knaust et al., 2023a Pakri Väikeküla outcrop
- Knaust et al., 2023a Mouth of the Lynna River Volkhov Stage
- Knaust et al., 2023a Ülemiste 29 borehole
- Knaust et al., 2023a Sõjamägi
- Knaust et al., 2023a Alliku quarry, Harjumaa
- Knaust et al., 2023a Vasalemma quarry
- Knaust et al., 2023a Mõdriku 39 borehole (Rakvere)
- Knaust et al., 2023a Nabala
- Knaust et al., 2023a Aulepa quarry
- Knaust et al., 2023a Saxby shore Vormsi Stage
- Knaust et al., 2023a Hosholm shore Pirgu Stage
- Knaust et al., 2023a Sarve harbour
- Knaust et al., 2023a Reinu Quarry
- Knaust et al., 2023a Valgu outcrop Adavere Stage
- Knaust et al., 2023a Suuriku cliff
- Knaust et al., 2023a Sepise outcrop
- Knaust et al., 2023a Kaugatuma-Lõo outcrop (ripple-mark coast)
- Knaust et al., 2023a Syass River, Rebrovo, Leningrad District Volkhov Stage