1-20 OF 37 RESULTS FOR

Thalassinoides suevicus

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Image
FIGURE 2 — Mecochirus rapax – <b>Thalassinoides</b> <b>suevicus</b>  association from the...
in > PALAIOS
Published: 01 January 2007
FIGURE 2 — Mecochirus rapax – Thalassinoides suevicus association from the Boca do Chapim Formation. A) Fallen slab with 28 nearly complete specimens of Mecochirus within or near Thalassinoides burrow maze; most of these specimens have since vanished due to illegal collecting at this site
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1983
AAPG Bulletin (1983) 67 (3): 430.
... not been clear, therefore, to what extent trace fossils preserved in flint zones are present at flintless zones. For example, in flint-bearing sequences, was the formation of beds of “thalassinoid” flints restricted in any degree to horizons especially bioturbated with Thalassinoides suevicus? Conversely...
Journal Article
Published: 01 June 1985
Canadian Journal of Earth Sciences (1985) 22 (6): 801–828.
...., Thalassinoides paradoxicus , Thalassinoides suevicus , Trichichnus linearis , Zoophycos sp., and mineralized burrows. Minor forms include Palaeophycus sp., Rosselia spp., and mantled burrows.Characteristic trace fossil distributions especially include the striking dominance of Thalassinoides paradoxicus in chalk...
Journal Article
Journal: PALAIOS
Published: 01 January 2007
PALAIOS (2007) 22 (1): 104–109.
...FIGURE 2 — Mecochirus rapax – Thalassinoides suevicus association from the Boca do Chapim Formation. A) Fallen slab with 28 nearly complete specimens of Mecochirus within or near Thalassinoides burrow maze; most of these specimens have since vanished due to illegal collecting at this site...
FIGURES
Image
TABLE 1 —Table comparing  <b>Thalassinoides</b> <b>suevicu</b> .,  Psilonichnus tubiformi...
in > PALAIOS
Published: 01 April 2000
TABLE 1 —Table comparing Thalassinoides suevicu ., Psilonichnus tubiformi ., Psilonichus upsilo ., and the traces described in this paper. The different trace fossils are compared on the basis of the diagnosis, their occurrence, and potential tracemakers
Journal Article
Journal: PALAIOS
Published: 16 January 2018
PALAIOS (2018) 33 (1): 29–35.
... (xylic substrates). This study provides several examples of morphologies of Glossifungites saxicava from the Campanian Sunnyside Coal (Blackhawk Formation) that exhibit both xenoglyphs and bioglyphs. Glossifungites along this surface are locally present as compound ? Thalassinoides suevicus...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.252.01.09
EISBN: 9781862395008
... level of laminated shales to Chondrites bioturbation typical of anoxic–suboxic conditions; (4) that Thalassinoides suevicus is commonly developed in micritic limestone and carbonated sands units throughout the section. Interpretation of the palaeo-oxygenation of this section on the basis of trace...
FIGURES | View All (8)
Journal Article
Published: 01 March 1984
Journal of Paleontology (1984) 58 (2): 298–311.
... silicified within the flint. Thalassinoides suevicus is the most commonly silicified trace fossil in chalk, generally preserved as a replacement of the burrow fill. Bathichnus paramoudrae typically is unsilicified but is encircled by ring-like paramoudra flints. Other trace fossils (e.g., Chondrites...
Image
FIGURE 7 —Invertebrate trace fossils from La Posa. (A)  <b>Thalassinoides</b> suev...
in > PALAIOS
Published: 01 August 2001
FIGURE 7 —Invertebrate trace fossils from La Posa. (A) Thalassinoides suevicus . (B) Ophiomorpha nodosa
Journal Article
Published: 01 November 2002
Journal of Sedimentary Research (2002) 72 (6): 871–883.
... consists of poorly defined tubular burrows, probably Thalassinoides ( Fig. 3B ). Facies 2B is crosscut by rhizoliths that descend from the overlying lignite (F3A), and by well-defined, unlined Thalassinoides suevicus that crosscut F3A and F2B. Santa Julia A is ultimately capped by the aforementioned...
FIGURES | View All (5)
Journal Article
Published: 01 June 2010
Bulletin of Canadian Petroleum Geology (2010) 58 (2): 115–140.
... interpreted as offshore transition include Aulichnites, Conichnus, Cruziana, Diplichnites , Fustiglyphus, Halopoa , Helminthopis, Lockeia , Monomorphichnus , Palaeophycus, Planolites, Protovirgularia, Rhizocorallium, Rusophycus , Spongeliomorpha, Thalassinoides and Treptichnus . Although trace fossil...
FIGURES | View All (12)
Journal Article
Journal: PALAIOS
Published: 01 December 2004
PALAIOS (2004) 19 (6): 551–564.
..., trace-makers of Thalassinoides suevicus can rework the uppermost 75 cm of the intertidal zone in less than a year ( MacGinitie, 1934 ; Warme, 1967 ). This is significant because ichnofabric indices of the Thalassinoides beds in the Virgin limestone reach a maximum of 3, indicating...
FIGURES | View All (7)
Series: SEPM Special Publication
Published: 01 January 2007
DOI: 10.2110/pec.07.88.0223
EISBN: 9781565762909
... and dwelling of crustaceans and perhaps worm-like animals can be assumed for R. commune, R. irregulare, and R. uliarensis, whereas R. jenense also could be the result of the activity of insects (e.g. mayflies; cf. Fürsich and Mayr, 1981 ). FIG. 9. Thalassinoides suevicus , preserved in hyporelief...
FIGURES | View All (12)
Image
FIGURE 3 —Reconstruction of  Mecochirus rapax . A) In its burrowing life mo...
in > PALAIOS
Published: 01 January 2007
FIGURE 3 —Reconstruction of Mecochirus rapax . A) In its burrowing life mode. B) Predominantly horizontal Thalassinoides suevicus burrow systems showing two successive event levels, with Mecochirus in life position (artwork by Carlos Farinha)
Image
Glossifungites  burrows and associated traces.  A )  Glossifungites  at the...
in > PALAIOS
Published: 16 January 2018
form (Gc) at the termination of a ? Thalassinoides suevicus (Th), with Teredolites longissimus (Tl). C ) Base of sandstone with Radichnus isp. (Rd) (purple arrows = scratches), Teredolites clavatus (Tc), ? Thalassinoides suevicus (red arrows = linear features that are possibly xenoglyphs
Image
Relative frequencies of the ichnospecies from the Abad Member of the Vera B...
Published: 12 April 2017
x majus xx miocenicum x x gomezi x xx intermedium xxx xxx x minimum xxx Phycodes bilix x Scolicia prisca x plana xx Thalassinoides suevicus x Urohelminthoida dertonensis
Image
Ichnofossils from the Abad Member, Vera Basin. (a)  Helminthoida labyrinthi...
Published: 12 April 2017
hyporelief on the base of a 1.1 cm thick, medium-grained sandstone. (c) Circulichnis montanus (C) and Helminthoida labyrinthica (Hl) preserved in convex hyporelief on the base of a 1.8 cm thick, medium-grained sandstone. (d) Thalassinoides suevicus (T) preserved in convex hyporelief on the base of a 3
Image
Various trace fossils in the Stirone section corresponding to clusters. A) ...
in > PALAIOS
Published: 01 September 2011
bioturbated background, cluster 8, lower unit. E) Scolicia isp. (Sc) penetrating along the top of muddy-silty intercalations, cluster 16, upper unit. F) Spongeliomorpha isp. (Sp), lower unit, detail of cluster 5. G) Thalassinoides cf. suevicus (Th) with concretional overgrowth and Ophiomorpha nodosa (Oph
Journal Article
Journal: PALAIOS
Published: 01 April 2011
PALAIOS (2011) 26 (4): 212–224.
... with the postdepositional nature of the specimens reported here. Wetzel's specimen is a true network with the hexagonal mesh interlocking (albeit in an eroded state due to the predepositional nature of the trace). Several specimens of Thalassinoides suevicus were identified in this study that share characteristics...
FIGURES | View All (8)
Image
Highly bioturbated silty/muddy sandstone, lithofacies L-V, Kahntah River Fi...
Published: 01 June 2010
), well C-040-C/94-I-02, 686.8 m. This photograph illustrates a common facies relationship between lithofacies L-V and L-III. E. Rosellia socialis, Palaeophycus tubularis and Thalassinoides cf. T. suevicus , well C-040-C/94-I-02, 683.1 m. F. Diplocraterion helmerseni , well A-081-A/94-I-03, 670.6 m.