<i>Terebellina mackayi</i>Bather in Oretian Murihiku rocks, Wairaki Hills, Southland

Begg, John; Cave, Murry; Campbell, John

doi:10.1080/00288306.1983.10421528

Cited by 10 publications

(12 citation statements)

References 5 publications

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“…Other brachiopods Misolia misolica described by Seidlitz (1913) from Misool are very close to Buru (Fogi Beds) (Boehm, 1908 Jaworski (1915), then by Wanner (1931), and lately by Hasibuan (1991Hasibuan ( , 2007b from the same area. Terebellina mackayi was first described by Bather (1905) from New Zealand and its age ranges possibly from Ladinian to Norian (Campbell and Waren, 1965;Force and Force, 1978;Begg et al, 1983). The species probably also occur in Thailand within Carnian strata and Ladinian strata with Daonella in Malaysia (Grant-Mackie pers.…”

Section: Discussionmentioning

confidence: 99%

The Triassic Marine Biota of Eastern Indonesia and its Interregional and Global Correlation: A Review

Hasibuan¹

2010

Indonesian J. Geosci.

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Section: Discussionmentioning

confidence: 99%

The Triassic Marine Biota of Eastern Indonesia and its Interregional and Global Correlation: A Review

Hasibuan¹

2010

Indonesian J. Geosci.

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“…obs.). The northeastern boundary of the andesite is faulted, bringing it into contact with sediments of probable Etalian (early Middle Triassic) age (Begg 1981). Sandstones near here have a low dip (15°, 04°W) and the andesite body may be essentially horizontal.…”

Section: Moss Bog Areamentioning

confidence: 99%

“…A flow foliation with 30° southeast dip is essentially parallel to bedding of Oretian sandstones, mudstones, and pebble beds (Mutch 1964;Begg 1981) which are exposed in a large quarry above the road and at the south end of the road cutting. The contact between andesite and sedimentary rocks is complexly faulted, but original emplacement of the andesite was probably concordant with bedding.…”

Section: Field Relationsmentioning

confidence: 99%

“…2 and Gowan Hill Station (4 km northeast and 5 km north, respectively, of Moss Bog) sheeted remnants of twopyroxene andesite, mostly with glassy groundmasses, dip gently northeast. They are associated with conglomerate within strata which contain Kaihikuan brachiopod faunas both above and below the andesites (Begg 1981 …”

Section: Gowan Hill No 2 Trig and Gowan Hill Station Near Gowanmentioning

confidence: 99%

“…It is enclosed within coarse sandstones, conglomerates, and siltstones which in the west have variable attitudes and are of Kaihikuan or Oretian age (Begg 1981;pers. obs.).…”

Section: Moss Bog Areamentioning

confidence: 99%

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The Park Volcanics group: Field relations of an igneous suite emplaced in the Triassic‐Jurassic Murihiku Terrane, South Island, New Zealand

Coombs

Cook

Campbell

1992

New Zealand Journal of Geology and Geophysics

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Examples of Mesozoic and CenozoicBathysiphon(Foraminiferida) from the Pacific Rim and the taxonomic status ofTerebellinaUlrich, 1904

Miller

1995

J. Paleontol.

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The generic name Terebellina was proposed by E. O. Ulrich for large (> 100 mm long, several millimeters wide), siliceous, tubular fossils from Cretaceous rocks of southern Alaska. Originally interpreted as annelid tubes, these unusual agglutinated fossils are locally abundant in Triassic to Neogene flysch and other basinal deposits of the Pacific borderlands. Other generic names employed for the same fossils include Torlessia (used in New Zealand) and Yokoia (in Japan). Although most authors have regarded the tubes as body fossils of worms, some workers have speculated recently that Pacific Terebellina are really large bathysiphonid foraminiferids. At the same time, the name has been co-opted by trace fossil workers for thick-walled, grain-lined burrows usually occurring in outer-shelf to slope facies.Based on comparisons with modern and fossil bathysiphonids, including a new species (Bathysiphon harperi) from the Cretaceous of southwestern Oregon, the body fossils called Terebellina are here reinterpreted as large species of Bathysiphon, and the name Terebellina is therefore a junior synonym of this foraminiferid genus. Except for the compression and recrystallization of tubes, Pacific Terebellina resemble very closely the tests of larger species of modern Bathysiphon. Terebellina should not be salvaged for use as an ichnogenus. Most of the trace fossils identified with this name in the recent literature could be accommodated in other established ichnogenera, primarily Palaeophycus (where grain-lined burrows occur individually and are dominantly horizontal) and Schaubcylindrichnus (where they occur in curved bundles).

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Terebellina mackayiBather in Oretian Murihiku rocks, Wairaki Hills, Southland

Cited by 10 publications

References 5 publications

The Triassic Marine Biota of Eastern Indonesia and its Interregional and Global Correlation: A Review

The Triassic Marine Biota of Eastern Indonesia and its Interregional and Global Correlation: A Review

The Park Volcanics group: Field relations of an igneous suite emplaced in the Triassic‐Jurassic Murihiku Terrane, South Island, New Zealand

Examples of Mesozoic and CenozoicBathysiphon(Foraminiferida) from the Pacific Rim and the taxonomic status ofTerebellinaUlrich, 1904

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