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Isopodichnus

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FIGURE 9 —Ranges of selected arthropod-derived trace fossils and of selecte...
Published: 01 October 2002
FIGURE 9 —Ranges of selected arthropod-derived trace fossils and of selected species of Cruziana . Cruziana range includes that of Isopodichnus (see text). “ Isopodichnus ” is not shown separately, but is included with Cruziana in the ichnogenus column and with Cruziana tenella
Journal Article
Journal: PALAIOS
Published: 01 October 2002
PALAIOS (2002) 17 (5): 435–448.
...FIGURE 9 —Ranges of selected arthropod-derived trace fossils and of selected species of Cruziana . Cruziana range includes that of Isopodichnus (see text). “ Isopodichnus ” is not shown separately, but is included with Cruziana in the ichnogenus column and with Cruziana tenella...
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Journal Article
Published: 01 October 1979
Canadian Journal of Earth Sciences (1979) 16 (10): 2022–2039.
... , Isopodichnus , Palaeophycus , Planolites , ? Rhizocorallium cf. R . irregulare , Rusophycus , Teichichnus cf. rectus , Tomaculum and Trichichnus are described in detail. Miscellaneous traces, those not morphologically distinct and (or) sufficiently abundant to warrant formal taxonomic treatment, are briefly...
Journal Article
Published: 01 December 1978
Journal of Sedimentary Research (1978) 48 (4): 1111–1127.
...L. B. Clemmensen Abstract The Middle Triassic Edderfugledal Member of East Greenland is interpreted as lacustrine because of: (A) nonmarine fossils such as conchostracans and small bivalves, (B) non-marine trace fossils such as Isopodichnus , Cruziana , Pelecypodichnus and Fuersichnus , (C...
Journal Article
Published: 01 May 2002
Journal of Paleontology (2002) 76 (3): 546–557.
... produced by crustaceans. Several slabs are covered with hundreds of tiny isolated bilobed resting traces, 1–3 mm long, similar to Isopodichnus minutus Debriette and Gand, 1990, which were probably produced by very small crustaceans or ostracodes. Other rare invertebrate traces consist of paired...
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Figure  12 —Bioturbation intensity:  1,  rippled sandstone beds with slight...
Published: 01 November 2006
Figure 12 —Bioturbation intensity: 1, rippled sandstone beds with slight bioturbation (BI = 1–3); 2, moderate bioturbation with abundant Isopodichnus isp. (BI = 3); 3, high bioturbation (BI = 4); 4, very high bioturbation (BI = 5). All examples come from the Presto-El Peral section
Journal Article
Published: 01 November 2006
Journal of Paleontology (2006) 80 (6): 1205–1226.
...Figure 12 —Bioturbation intensity: 1, rippled sandstone beds with slight bioturbation (BI = 1–3); 2, moderate bioturbation with abundant Isopodichnus isp. (BI = 3); 3, high bioturbation (BI = 4); 4, very high bioturbation (BI = 5). All examples come from the Presto-El Peral section...
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Figure  3 — 1,  Lockeia siliquaria  James, 1879 ;  2,  L. siliquaria , note...
Published: 01 November 2006
Figure 3 — 1, Lockeia siliquaria James, 1879 ; 2, L. siliquaria , note the specimen just at the end of a sinuous furrow (arrow); 3, Rusophycus isp.; 4, Isopodichnus problematicus Schindewolf, 1928 ; 5, Protovirgularia rugosa ( Miller and Dyer, 1878 ); 6, ?trilobite resting trace; 7
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Figure  6 — Quadrispinichna parvia  n. igen. and isp., (type 1).  1,  Holot...
Published: 01 May 2002
Figure 6 — Quadrispinichna parvia n. igen. and isp., (type 1). 1, Holotype, SAM 3547, ×0.70; 2, SAM 6494, poorly preserved Q. parvia associated with trail and isolated Isopodichnus isp., ×0.60; 3, paratype, SAM 11605, ×0.65; 4, paratype, SAM 11607, ×0.65; 5, paratype, SAM 11604
Journal Article
Journal: PALAIOS
Published: 01 February 1988
PALAIOS (1988) 3 (1): 53–68.
... not cluster well because complex, overlapping environmental gradients occur in nearshore facies (Rhoads, 1975; Frey and Pemberton, 1984, p. 199; Howard and Frey, 1984). The NTSYS statistical package (Rohlf et al., 1974; Rohlf, 1985) used the unweighted pair-group average method (Davis, Isopodichnus Rest...
Journal Article
Published: 01 December 1981
Journal of the Geological Society (1981) 138 (6): 675–694.
... Sediment Transport and Environmental Management 1976 New York Wiley 311 50 Trewin N. H. Isopodichnus in a trace fossil assemblage from the Old Red Sandstone Lethaia 1976 9 29 37 Trewin N. H. Transported graptolites and associated tool marks from Grieston Quarry...
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Table 1 —Ichnoassemblage composition (“1” presence, “0” absence) of Upper S...
Published: 01 April 2001
, Isopodichnus and Tumblagoodichnus ), 4 Petalichnus , 5 Small horizontal meandering (looping) trails (e.g., Mermia , Gordia ), 6 Arthropod resting traces (i.e., Selenichnites and Rusophycus ), 7 Merostomichnites , 8 Siskemia , 9 Grazing trails (i.e., “epichnial ridge” of Bradshaw [1981
Journal Article
Published: 01 March 2008
Geological Magazine (2008) 145 (2): 301.
... was synonymized with Ophiomorpha annulata Ksiazkiewicz by Uchman (1995) ; Muensteria is used instead of the generally accepted Taenidium (but D’Alessandro & Bromley (1987 ) is listed in the references); and Isopodichnus is used instead of Rusophycus (while Bromley & Asgaard (1972 ) is listed...
Journal Article
Published: 01 August 2017
Journal of Paleontology (2017) 91 (5): 987–993.
..., but can be abundant on some bedding surfaces (Isbell et al., 2001 ). Arthropod-produced traces are represented by a single ichnogenus— Isopodichnus , which is a feeding trace generally attributed to concostracan crustaceans (Pollard, 1985 ). No arthropod-produced walking trails have been reported from...
Journal Article
Published: 01 April 2021
Journal of the Geological Society (2021) 178 (4): jgs2020-233.
... elements in their morphologies. In contrast to inorganic sedimentary structures, the T1 traces have a similar morphology to the ‘short resting trace’ type described from the Lower Stromness Flags of Orkney, although these are half the size and are part of an Isopodichnus ( =  Rusophycus ) assemblage...
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Journal Article
Published: 01 May 2011
Journal of Paleontology (2011) 85 (3): 502–518.
... ) are not similar to the bilobate ornamented structures described herein. In any case, the ichnogenus Isopodichnus which has been used in the past to refer to small bilobate hyporeliefs (now included in the ichnogenus Cruziana and Rusophycus) has often been attributed to isopods (e.g., Pollard, 1985 ; Gingras et...
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Journal Article
Published: 01 November 2000
Scottish Journal of Geology (2000) 36 (2): 151–158.
... Isopodichnus of probable arthropod origin. An early Devonian ichnofauna from the Ousdale Mudstones includes seven genera probably produced by arthropods ( Trewin 1993 b ), and other arthropod-related traces are known from the Moray Firth Coast ( Trewin and Kneller 1987 ; Carroll 1990 ). Three groups...
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Journal Article
Published: 01 December 1997
Bulletin of Canadian Petroleum Geology (1997) 45 (4): 553–575.
... of facies G and is abruptly overlain by the cryptalgal laminated carbonate mudstone of facies I. Facies H is characterized by a moderately diverse Psilonichnus trace fossil assemblage (Frey and Pemberton, 1985), consisting of Skolithos, Palaeophycus, Isopodichnus and an, as yet, undescribed type of bivalve...
Journal Article
Journal: PALAIOS
Published: 01 February 2006
PALAIOS (2006) 21 (1): 46–62.
..., and the appendage imprints have negative epirelief. Brady (1947) recorded Oniscoidichnus (as “ Isopodichnus Brady 1947 ”) from the same ichnofossil assemblage as Paleohelcura —this also is the case with the Ringerike samples. Three specimens of Oniscoidichnus have been found, all within very fine-grained...
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Series: Text Book
Published: 01 January 2022
DOI: 10.17491/bgsi.2022.9859.05
EISBN: 9789380998596
...)   Rusophycus didymus (scale = 1.0 cm); (C)   Rusophycus didymus (scale = 1.0 cm); (D)   Chondrites isp. (diameter of coin = 2.0 cm); (E)   Cruziana isp. (diameter of coin = 2.3 cm); (F)   Cruzian a isp. (close up view) (scale = 1.0 cm); (G)   Isopodichnus isp. (scale = 1.0 cm); (H)   Isopodichnus...
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