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104:
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may have been undertracks that penetrated to the underlying layer of sediment, and the fossil trackways thus produced on the top surface (preserving the impression of the dragging tail) were
227:
with two parallel rows of blunt to elongate, closely spaced tracks oriented approximately perpendicularly to the mid-line of the trackway. The term is more often used for the
828:
188:
815:
642:
Hoxie, C. T. (2005). "Late
Cambrian arthropod trackways in subaerially exposed environments: Incentives to simplify a problematic ichnogenus".
493:
Collette, J. H.; J. W. Hagadorn (2010). "Three-dimensionally preserved arthropods from
Cambrian Lagerstatten of Quebec and Wisconsin".
251:
were produced by a fish “walking” in shallow water on pectoral or ventral fin spines. Previous to this he had suggested that a large
856:
447:
Briggs, D. E. G.; W. D. I. Rolfe & J. Brannan (1979). "A giant myriapod trail from the
Namurian of Arran, Scotland".
384:
464:
unshelled? Experimental model-based neoichnology and new evidence for a euthycarcinoid affinity for this ichnospecies".
129:
552:"Notice of the discovery of additional remains of land animals in the Coal-Measures of the South Joggins, Nova Scotia"
124:
694:
Woolfe, K. J. (1990). "Trace fossils as paleoenvironmental indicators in the Taylor Group (Devonian) of
Antarctica".
583:
Dawson, J. W. (1873). "Impressions of footprints of aquatic animals and imitative markings, on
Carboniferous rocks".
115:
from the
Joggins Formation (Pennsylvanian), Cumberland Basin, Nova Scotia. This trackway was made by the myriapod
308:
intertidal and subaerial deposits of North
America, especially the Potsdam and Elk Mound Groups, were produced by
267:) could have made them. Subsequent evidence has supported this earlier interpretation. The fossils on which this
861:
751:
739:
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population in the Moyer Ridge Member of the
Bloomsberg Formation (Late Silurian)-Snyder County, Pennsylvania".
231:
of this description; however, similar trackways from recent arthropods are sometimes given this name as well.
744:
288:
In the decades following Dawson's work, the trackways of several other arthropods were also included within
244:
783:
629:
Goldring, R.; A. Seilacher (1971). "Limulid undertracks and their sedimentological implications".
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strata of Nova Scotia, when Sir J. W. Dawson named it in 1873. Dawson proposed that
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deposits around the world. In addition, recent evidence indicates that some
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This type of trackway was originally based on large fossils from
781:
653:"Skimming the surface with Burgess Shale arthropod locomotion"
271:
was based are now thought to be from giant myriapods, such as
754:– "Nova Scotia, Carboniferous Geology and Paleontology"
631:
Neues
Jahrbuch für Geologie und Paläontologie, Abhandlungen
612:
Garlock, T. L.; P. E. Isaacson (1977). "An occurrence of a
657:
Proceedings of the Royal
Society B: Biological Sciences
651:
Minter, N. J.; M. G. Mángano & J.-B. Caron (2011).
460:
Collette, J. H.; Gass, K. C.; Hagadorn, J. W. (2012). "
522:
Davis, R. B.; N. J. Minter & S. J. Braddy (2007).
556:
Quarterly Journal of the Geological Society of London
790:
204:. These may have been made by the euthycarcinoid,
386:New Zealand Journal of Geology and Geophysics 1981
696:Palaeogeography, Palaeoclimatology, Palaeoecology
531:Palaeogeography, Palaeoclimatology, Palaeoecology
389:. Science Information Division, DSIR. p. 639
774:– 3-main types of trilobite trace fossils
281:could have been the result of a 1-meter-long
8:
524:"The neoichnology of terrestrial arthropods"
778:
102:
20:
676:
211:, which is also found at Blackberry Hill.
330:
196:from the Elk Mound Group (Cambrian),
7:
111:Oblique bedding plane view of large
758:Video--Euthycarcinoid animation on
732:arthropod trackway--(marine, tidal)
415:Collette, Gass & Hagadorn, 2012
14:
568:10.1144/GSL.JGS.1862.018.01-02.10
16:Ichnogenus of Arthropod trackways
128:
762:slab (Milwaukee Public Museum)
424:Goldring & Seilacher, 1971
296:, which are known from marine
1:
406:Collette & Hagadorn, 2010
708:10.1016/0031-0182(90)90139-X
543:10.1016/j.palaeo.2007.07.013
585:American Journal of Science
125:Trace fossil classification
878:
312:. In that scenario, the
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110:
101:
23:
740:Kansas Geological Survey
738:– "Bulletin 241",
383:Robert P. Lynch (1981).
857:Arthropod trace fossils
772:Trilobite Trace Fossils
644:Unpublished B.A. Thesis
495:Journal of Paleontology
466:Journal of Paleontology
304:trackways from certain
279:Diplichnites cuithensis
669:10.1098/rspb.2011.1986
597:10.2475/ajs.s3-5.25.16
550:Dawson, J. W. (1862).
212:
191:
462:Protichnites eremita
730:Diplichnites gouldi
663:(1733): 1613–1620.
373:Briggs et al., 1979
337:Minter et al., 1986
767:Trilobite Tracks:
346:Davis et al., 2007
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784:Taxon identifiers
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391:. Retrieved
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364:Dawson, 1862
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355:Dawson, 1873
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319:Protichnites
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314:Diplichnites
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302:Diplichnites
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290:Diplichnites
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274:Arthropleura
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257:annelid worm
249:Diplichnites
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237:Diplichnites
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229:ichnofossils
217:Diplichnites
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209:macnaughtoni
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194:Diplichnites
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176:Diplichnites
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168:Ichnogenus:
117:Arthropleura
116:
113:Diplichnites
112:
25:Diplichnites
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18:
433:Hoxie, 2005
263:(such as a
851:Categories
637:: 422–442.
624:: 282–287.
455:: 273–291.
393:2022-08-21
326:References
294:trilobites
269:ichnotaxon
253:crustacean
200:, central
162:Arthropoda
605:130625563
576:128483390
515:130064618
486:129234373
298:Paleozoic
285:walking.
265:millipede
225:trackways
222:arthropod
202:Wisconsin
148:Kingdom:
142:Eukaryota
807:Q5279813
801:Wikidata
687:22072605
614:Cruziana
306:Cambrian
261:myriapod
207:Mosineia
158:Phylum:
152:Animalia
138:Domain:
834:1034551
821:4805756
752:Article
736:Article
728:Photo--
678:3282348
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829:IRMNG
601:S2CID
572:S2CID
527:(PDF)
511:S2CID
482:S2CID
816:GBIF
683:PMID
235:The
220:are
37:Preęž’
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