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Campbellton Formation

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Journal Article
Journal: PALAIOS
Published: 01 June 2012
PALAIOS (2012) 27 (6): 424–438.
...KIRSTEN L KENNEDY; PATRICIA G GENSEL; MARTIN R GIBLING Abstract The Paleozoic spread of plants, beginning in the Ordovician and reaching a phase of accelerated diversity and dispersal in the Early Devonian, was a critical episode in Earth history. The Lower Devonian (Emsian) Campbellton Formation...
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Journal Article
Published: 10 November 2011
Canadian Journal of Earth Sciences (2011) 48 (12): 1561–1580.
...Kirsten Kennedy; Martin R. Gibling Abstract Strata of the Campbellton Formation, nearly 1 km-thick and known for its diverse fossil assemblage of early plants, arthropods, and fish, can be divided into six facies associations: (1) restricted lacustrine, (2) marginal lacustrine, (3) near-shore...
Image
Articulated  Doliodus  specimen NBMG 10127 from the <b>Campbellton</b> <b>Formation</b>, ...
Published: 24 October 2017
Fig. 2. Articulated Doliodus specimen NBMG 10127 from the Campbellton Formation, New Brunswick. (A) Whole specimen, immersed in ethanol, dorsal view. (B) Reconstruction, ventral view, based on 3D scan images (see Maisey et al. 2017 ); prepectoral and dorsal spines buried in matrix
Image
Photomicrographs of petrographic samples from the <b>Campbellton</b> <b>Formation</b> ori...
Published: 01 December 2013
Fig. 8.— Photomicrographs of petrographic samples from the Campbellton Formation oriented perpendicular to bedding (left in reflected white light, right in UV fluorescent light). Couplets of thick-walled cutinite (C) surround an inorganic mineral filling (m), and alternate with bands
Image
Geologic map of the <b>Campbellton</b> <b>Formation</b> and surroundings showing location...
in > PALAIOS
Published: 01 June 2012
FIGURE 1— Geologic map of the Campbellton Formation and surroundings showing locations of sections and major fossil localities. Geology from Wilson et al. (2004) . Roman numerals in circles on main figure represent sections I–VI, and numbers in pentagons on the inset map refer to stratigraphic
Image
Summary sections of all <b>Campbellton</b> <b>Formation</b> strata (from  Kennedy and Gib...
in > PALAIOS
Published: 01 June 2012
FIGURE 3— Summary sections of all Campbellton Formation strata (from Kennedy and Gibling, 2011 ). Facies Associations (FA) codes are listed in Table 1 . All sections are independent of each other, except for sections III and VI, between which a gap of 650 m was estimated assuming constant dips
Image
Summary of the facies associations of the <b>Campbellton</b> <b>Formation</b> and the gen...
in > PALAIOS
Published: 01 June 2012
T able 1— Summary of the facies associations of the Campbellton Formation and the genera found within.
Image
Examples of fossilization within the <b>Campbellton</b> <b>Formation</b>. A) An impressio...
in > PALAIOS
Published: 01 June 2012
FIGURE 4— Examples of fossilization within the Campbellton Formation. A) An impression of a dermal plate fragment of a fish (at right) in the mudstone matrix of the breccia unit near Atholville, New Brunswick. Ostracods are circled. B) Finely laminated coaly layers from section III showing dark
Journal Article
Published: 24 October 2017
Canadian Journal of Earth Sciences (2017) 54 (12): 1248–1262.
...Fig. 2. Articulated Doliodus specimen NBMG 10127 from the Campbellton Formation, New Brunswick. (A) Whole specimen, immersed in ethanol, dorsal view. (B) Reconstruction, ventral view, based on 3D scan images (see Maisey et al. 2017 ); prepectoral and dorsal spines buried in matrix...
FIGURES | View All (9)
Journal Article
Published: 18 May 2004
Canadian Journal of Earth Sciences (2004) 41 (5): 527–551.
... Formation. The Chaleurs Group is conformably overlain by Lochkovian to early Emsian subaerial volcanic rocks of the Dalhousie Group (Val d’Amour Formation), which is unconformably overlain by alluvial–lacustrine deposits of the late Emsian Campbellton Formation. Acadian orogenesis began during the Emsian...
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Journal Article
Published: 01 December 2013
Journal of Sedimentary Research (2013) 83 (12): 1202–1215.
...Fig. 8.— Photomicrographs of petrographic samples from the Campbellton Formation oriented perpendicular to bedding (left in reflected white light, right in UV fluorescent light). Couplets of thick-walled cutinite (C) surround an inorganic mineral filling (m), and alternate with bands...
FIGURES | View All (10)
Journal Article
Journal: GSA Bulletin
Published: 01 January 1975
GSA Bulletin (1975) 86 (1): 105–108.
...MARSHALL KAY Abstract The Campbellton sequence of probable Cambrian and early Ordovican age lies south of the Loon Bay batholith, which intrudes the Dunnage Melange on the north. The Loon Harbour Formation at the base of the sequence consists of hundreds or thousands of meters of volcanic rocks...
Journal Article
Published: 01 December 1971
Canadian Journal of Earth Sciences (1971) 8 (12): 1603–1605.
..., and is older than the Atholville Beds near Campbellton, N.B. La présence d'un petit Ptéraspidide est signalée pour la première fois dans la Formation dévonienne inférieure de Dalhousie, à Dalhousie, N.B. Ceci appuie la thèse voulant que cette formation soit d'une part, corrélative à une séquence de lits...
Journal Article
Published: 01 August 1968
Canadian Journal of Earth Sciences (1968) 5 (4): 945–953.
...D. L. Dineley; B. P. J. Williams Abstract The Devonian continental rocks outcropping between Campbellton, New Brunswick and Miguasha, Quebec are regrouped on the basis of new stratigraphic information and the ages now suggested are thought to be in accord with new data. An Early or early Middle...
Journal Article
Published: 12 December 2011
Canadian Journal of Earth Sciences (2012) 49 (1): 222–238.
..., the Chaleur Bay Synclinorium is underlain by Aeronian to lower Lochkovian rocks of the Chaleurs Group and Lower Devonian rocks of the Dalhousie and Tobique groups and Campbellton Formation. The focus of this paper is the Chaleurs Group, which conformably overlies the Matapédia Group on the west side...
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Journal Article
Published: 01 May 2007
Journal of Paleontology (2007) 81 (3): 588–590.
... Agassiz (Eurypterida: Devonian) from the Campbellton Formation, New Brunswick : Atlantic Geology , 32 . 95 – 100 . Nieszkowski , J. , 1859 , Der Eurypterus remipes aus den obersilurischen Schichten der Insel Oesel : Archiv für die Naturkunde Liv-, Ehst und Kurlands , 2 . 299 – 344...
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Journal Article
Published: 01 November 2010
Journal of Paleontology (2010) 84 (6): 1206–1208.
... as a juvenile eurypterid and its implications for scorpion systematics : Progressive Palaeontology Programme and Abstracts , 19 . Miller , R. F. , 2007 , Pterygotus anglicus Agassiz (Chelicerata: Eurypterida) from Atholville, Lower Devonian Campbellton Formation, New Brunswick, Canada...
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Journal Article
Published: 27 May 2004
Canadian Journal of Earth Sciences (2004) 41 (5): 587–602.
... Newfoundland. Formally described herein and named Red Island Road Formation, the strata represent a unique lithologic formation not exposed or known anywhere else in the region. Characteristic features include abundant, rounded, highly weathered and varnished cobbles and boulders derived from an unknown mixed...
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Journal Article
Published: 01 December 2006
Bulletin of Canadian Petroleum Geology (2006) 54 (4): 380–395.
... by a disconformity. The alluvial-lacustrine deposits of the upper Emsian Campbellton Formation ( Wilson et al., 2004 ) form the upper succession and unconformably overlie the Dalhousie Group. Finally, post-Acadian (post Middle Devonian) coarse-grained reddish sandstones and conglomerates of the Bonaventure Formation...
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Journal Article
Published: 01 December 2005
Bulletin of Canadian Petroleum Geology (2005) 53 (4): 454–471.
...D. Lavoie; G. Chi; P. Brennan-Alpert; A. Desrochers; R. Bertrand Abstract This study deals with the diagenetic evolution of dolostones of the Romaine Formation, from cores and outcrops on Anticosti and Mingan islands, and reports evidence for hydrocarbon migration in secondary porosity generated...
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