A checklist of marine algae of eastern Canada, second revision

1984 ◽  
Vol 62 (4) ◽  
pp. 680-704 ◽  
Author(s):  
G. Robin South
Keyword(s):  
New Brunswick ◽  
Marine Algae ◽  
The South ◽  
Eastern Canada ◽  
The North ◽  
Fucus Distichus ◽  
Anticosti Island

A revised checklist of 354 species, subspecies, and varieties of benthic marine algae from eastern Canada is given, consisting of 128 Rhodophyceae, 128 Phaeophyceae, 90 Chlorophyceae, 7 species of Vaucheria (Xanthophyceae), and 1 of Phaeosaccion (Chrysophyceae). Records for the entire coastline from Cape Chidley, Labrador, in the north to the New Brunswick – Maine border in the south are included, as well as from Anticosti Island, Magdalen Island, Sable Island, and St. Pierre and Miquelon. Additions include Waerniella lucifuga (Kuck.) Kylin; Phloeospora curta (Fosl.) Jaasund; Striaria attenuata (Grev.) Grev.; Fucus distichus L. subsp. anceps (Harv. et Ward ex Carm.) Powell (Phaeophyta); Pilinia ? rimosa Kütz.; and Tellamia contorta Batt. (Chlorophyta).

A checklist of marine algae of eastern Canada

1970 ◽  
Vol 48 (12) ◽  
pp. 2077-2095 ◽  
Author(s):  
G. Robin South ◽  
André Cardinal
Keyword(s):  
New Brunswick ◽  
Marine Algae ◽  
New Records ◽  
The South ◽  
Eastern Canada ◽  
The North ◽  
Anticosti Island

A checklist of 371 species, subspecies, and varieties of benthic marine algae from eastern Canada is given, consisting of 157 Rhodophyceae, 127 Phaeophyceae, and 87 Chlorophyceae. Records for the entire coastline from Cape Chidley, Labrador, in the north to the New Brunswick – Maine border in the south are included, as well as from Anticosti Island, Magdalen Island, Sable Island, and St. Pierre and Miquelon. Mikrosyphar porphyrae Kuck. and Protectocarpus speciosus (Børg.) Kuck. are new records for the area.

A comparison of magnetic character and alteration in three granite drill cores from eastern Canada

1988 ◽  
Vol 25 (8) ◽  
pp. 1141-1150 ◽  
Author(s):  
K. L. Harding ◽  
W. A. Morris ◽  
S. J. Balch ◽  
P. Lapointe ◽  
A. G. Latham
Keyword(s):  
Nova Scotia ◽  
New Brunswick ◽  
The South ◽  
Eastern Canada ◽  
General Observation ◽  
South Mountain Batholith ◽  
Magnetite Content ◽  
Bulk Magnetic Susceptibility ◽  
Primary Oxidation ◽  
Drill Cores

Bulk magnetic susceptibility (BMS) measurements have been made on granite drill cores from the St. George batholith (New Brunswick), the South Mountain batholith (Nova Scotia), and the Wedgeport pluton (Nova Scotia). The primary magnetite concentrations of the two Nova Scotia cores are statistically indistinguishable, thus lending support to the hypothesis that the Wedgeport pluton, despite being 50 Ma younger, is a satellite of the South Mountain batholith.The St. George core has a primary magnetite concentration over 30 times greater than the Nova Scotia cores, but low-temperature alteration (attributable to subsurface weathering) has greatly reduced its magnetite content. The two Nova Scotia S-type granites are shown to fall into the ilmenite-series category, whereas the St. George granite, which is either S- or A-type, is transitional between the magnetite and ilmenite series.The general observation of intergranular hematite and reduced BMS in the outcrops of some granites is suggested to have important consequences for primary oxidation studies and aeromagnetic interpretation.

scholarly journals La mer de Goldthwait au Québec

2010 ◽  
Vol 31 (1-2) ◽  
pp. 61-80 ◽  
Author(s):  
Jean-Claude Dionne
Keyword(s):  
Quebec City ◽  
The South ◽  
Lawrence Estuary ◽  
Marine Invasion ◽  
North Shore ◽  
The North ◽  
Upper Limit ◽  
South Shore ◽  
Anticosti Island ◽  
St Lawrence Estuary

The Goldthwait Sea is defined as the late- and post-Glacial marine invasion in the St. Lawrence Estuary and Gulf east of Québec City. In Québec, this sea has submerged an area of about 25 000 km2. The largest areas submerged are the north shore of the St. Lawrence between Les Escoumins and Blanc-Sablon, the south shore between Levis and Tourelles, and the Anticosti Island. The upper limit of the Goldthwait Sea varies from place to place. The Goldthwait Sea began 14 000 years ago and land emergence is still in progress, since the pre-Wisconsin marine level has not been recovered yet. For a better chronology, this long interval needs to be subdivided. Three main periods have been recognized: Goldthwaitian I, II and III. However, a geographical subdivision is also needed. Numerous shorelines were observed at various elevations throughout the area formely submerged by the Goldthwait Sea. However, only a few shorelines are well developed and extensive, and correlations between former shorelines are difficult to establish. Only three levels are widespead and common to the Estuary and parts of the Gulf. The isostatic recovery has been rapid during the first three thousand years after déglaciation of the area: about 75%.

The Mud-Dwelling Hydrozoan Boreohydra simplex in the Western North Atlantic

1974 ◽  
Vol 31 (10) ◽  
pp. 1666-1667
Author(s):  
Dale R. Calder
Keyword(s):  
North Atlantic ◽  
South Atlantic ◽  
The South ◽  
Eastern Canada ◽  
South Georgia ◽  
The North ◽  
The North Atlantic

Boreohydra simplex was collected at a depth of 400 m in Cabot Strait, eastern Canada; this solitary, mud-dwelling hydroid is previously unreported from the western North Atlantic. Elsewhere, it has been found along the coasts of Scandinavia, Britain, and Iceland in the North Atlantic, and from South Georgia in the South Atlantic.

Biostratigraphic significance of lower Paleozoic microfaunas from eastern Canada

2004 ◽  
Vol 41 (5) ◽  
pp. 489-505 ◽  
Author(s):  
Esther Asselin ◽  
Aïcha Achab ◽  
Azzedine Soufiane
Keyword(s):  
New Brunswick ◽  
Lower Devonian ◽  
Head Group ◽  
Upper Ordovician ◽  
Eastern Canada ◽  
Lower Paleozoic ◽  
Anticosti Island ◽  
Gaspe Peninsula ◽  
Gaspé Peninsula ◽  
Mapping Program

Chitinozoan studies recently carried out in the “Appalachian Forelands and St. Lawrence Platform” National Geoscience Mapping Program (NATMAP) project have confirmed the regional biostratigraphic value of a number of chitinozoan species and led to a better documentation of their stratigraphic and geographic distribution in eastern Canada. The typical Darriwilian microfaunas first described from the Table Head Group of western Newfoundland and containing Conochitina chydaea are now recognised in the Rivière Ouelle Formation at Les Méchins, Gaspé Peninsula. In the Upper Ordovician successions of the St. Lawrence Platform at Neuville and in the Charlevoix area, Quebec, Conochitina primitiva is indicative of the multidens–pre-americanus graptolite zonal range, Hercochitina duplicitas of the americanus Zone, and Hercochitina spinetum and Acanthochitina cancellata characterize the ruedemanni – lower spiniferus zonal interval. The occurrence of Cyathochitina vaurealensis and Hercochitina crickmayi in turbidite deposits of the Grog Brook Group of northwestern New Brunswick confirms the minimal facies dependence of these two Richmondian index species. Eisenackitina dolioliformis, characteristic of the late Aeronian and Telychian successions of Arctic Canada, Gaspé Peninsula, and Anticosti Island, is now recognised in samples from the Upsalquitch Formation of northwestern New Brunswick and the Cabano Formation of the Rimouski area in Quebec. The palynological data from Devonian successions of the Matapedia Valley, the Rimouski area, and the Beauce – Eastern Townships region show that the succession of Lower Devonian chitinozoan assemblages of the Forillon Peninsula based on short-ranging species can be used in establishing regional correlations in the Gaspé Belt.

scholarly journals Alethopteris and Neuralethopteris from the lower Westphalian (Middle Pennsylvanian) of Nova Scotia and New Brunswick, Maritime Provinces, Canada

2020 ◽  
Vol 56 ◽  
pp. 111-145
Author(s):  
Carmen Álvarez-Vázquez
Keyword(s):  
United States ◽  
Nova Scotia ◽  
New Brunswick ◽  
Western Europe ◽  
The United States ◽  
Maritime Provinces ◽  
Eastern Canada ◽  
Systematic Revision ◽  
Insufficient Attention ◽  
The North

A systematic revision of Alethopteris and Neuralethopteris from upper Namurian and lower Westphalian (Middle Pennsylvanian) strata of Nova Scotia and New Brunswick, eastern Canada, has demonstrated the presence of eight species: Alethopteris bertrandii, Alethopteris decurrens, Alethopteris cf. havlenae, Alethopteris urophylla, Alethopteris cf. valida, Neuralethopteris pocahontas, Neuralethopteris schlehanii and Neuralethopteris smithsii. Restudy of the Canadian material has led to new illustrations, observations and refined descriptions of these species. Detailed synonymies focus on records from Canada and the United States. As with other groups reviewed in earlier articles in this series, it is clear that insufficient attention has been paid to material reposited in Canadian institutions in the European literature. The present study emphasizes the similarity of the North American flora with that of western Europe, especially through the synonymies.

Stratigraphy and sedimentology of the Pennsylvanian Grande Anse Formation, Cumberland Basin, eastern Canada: its relationship to salt tectonics and coeval strata of the Joggins World Heritage Site

2020 ◽  
pp. 1-16
Author(s):  
Fadel Bahr ◽  
Dave Keighley
Keyword(s):  
Sedimentary Basins ◽  
World Heritage ◽  
World Heritage Site ◽  
Salt Tectonics ◽  
The South ◽  
Eastern Canada ◽  
Black Point ◽  
The North ◽  
Grande Anse ◽  
Hydrological System

The Cumberland Basin is one of several sedimentary basins composing the late Paleozoic Maritimes Basin complex of eastern Canada. Pennsylvanian salt tectonics in the Cumberland Basin caused two salt mini-basins to evolve on either side of the Minudie Anticline, a salt wall. South of the wall (Athol Syncline), along the Joggins World Heritage shoreline, an ∼3000 m succession of strata (Little River, Joggins, Springhill Mines, and Ragged Reef formations) accumulated conformably on the Boss Point Formation. North of the wall (Black Point sub-basin), the biostratigraphically equivalent, but mostly unstudied, ∼600 m thick succession of Grande Anse Formation lies in angular unconformity on folded and faulted Boss Point and basal Little River formations. Grande Anse Formation sedimentology indicates four lithofacies associations: floodplain (LA1), braided channel (LA2), sheet flood (LA3), and debris flow deposits (LA4). One possible model has the Black Point sub-basin with its own hydrological system, completely separated from the Athol Syncline. A low subsidence rate combined with the low sedimentation rate produced the ∼600 m thick sand- and mud-prone succession that was contemporaneous with the ∼3 km succession to the south. The second model proposes that north of the salt wall was exposed to erosion during accumulation of Joggins and Springhill Mines formation strata to the south. Subsequently, the sediment of the lithologically similar Ragged Reef and Grande Anse formations either (i) onlapped to the north, unconformably on the folded Boss Point; or (ii) unconformably–disconformably on the underlying strata after a period of time indistinguishable in the biostratigraphic record.

Analysis of the Primary and Secondary Control Networks of New Brunswick — Implications for a Readjustment to Satellite Control

1971 ◽  
Vol 25 (2) ◽  
pp. 144-155 ◽  
Author(s):  
E. Krakiwsky ◽  
G. Konecny
Keyword(s):  
New Brunswick ◽  
North American ◽  
Primary Control ◽  
Eastern Canada ◽  
Control Networks ◽  
First Order ◽  
The North ◽  
Triangulation Network ◽  
Simultaneous Adjustment ◽  
Method Of Adjustment

Various problems associated with the adjustment of geodetic control networks in Eastern Canada are discussed. Results of analyses of the primary control networks in New Brunswick indicate that significant distortions are present and are due mainly to the Bowie Method of adjustment used when the 1927 North American Datum was adopted. The “free adjustments” made by the authors show that the proportional accuracy can be improved from the present lowest value of 1:20,000 to as high as 1:200,000. Other analyses cited in the paper indicate that there may be merit in combining first- and second-order control networks in a simultaneous adjustment. Some details are given on merging the first-order terrestrial networks in Eastern Canada with one triangle of the North American satellite triangulation network in a simultaneous adjustment.

scholarly journals Paleotethyan faunal/floral evidence in the Mississippian Maritimes Basin of Canada: An overview

2021 ◽  
pp. 1-20
Author(s):  
Pedro Cózar ◽  
Ian D. Somerville
Keyword(s):  
Nova Scotia ◽  
North America ◽  
New Brunswick ◽  
Western Europe ◽  
Statistical Analyses ◽  
Eastern Canada ◽  
Rheic Ocean ◽  
The North ◽  
Logical Connection ◽  
Maritimes Basin

Abstract In this study, middle to late Mississippian microfossil assemblages from the Maritimes Basin of eastern Canada (Nova Scotia, SW Newfoundland, and New Brunswick) are closely compared to those from Western Paleotethys basins. The comparison is focused mainly on foraminifers and calcareous algae. Most foraminifers and algae described from the Maritimes Basin are considered cosmopolitan, and the occurrence in western Europe and northern Africa of taxa previously considered endemic to the North America Realm suggests a close paleobiogeographic relationship. This European/African correlation is further supported by other foraminiferal/algal taxa, the importance of which were previously overlooked, including: Plectogyranopsis ex gr. P. hirosei (Okimura, 1965), Mikhailovella Ganelina, 1956, Koktjubina windsorensis (Mamet, 1970), Polysphaerinella bulla Mamet, 1973, Mstinia Dain in Dain and Grozdilova, 1953, Haplophragmina Reitlinger, 1950, Omphalotis Shlykova, 1969, Pseudolituotuba Vdovenko, 1971, Pseudoendothyra Mikhailov, 1939, Saccamminopsis (Sollas, 1921) Vachard and Cózar, 2003, Kamaenella Mamet and Roux, 1974, and Anthracoporellopsis Maslov, 1956. Some species recorded in the Maritimes Basin have been typically recorded in Britain and Ireland in the southern platform of Laurussia. This implies a connection via the Rhenohercynian Ocean, whereas statistical analyses suggest that Maritimes Basin assemblages are closer to those of the Gondwana platform, which could have been established via the Paleotethys Ocean, and also with terranes northwest of the Variscan Front, in which its most logical connection should be with a still-open Rheic Ocean during the Visean and early Serpukhovian. Those taxa demonstrate a more-or-less continuous faunal and microfloral interchange between the Maritimes Basin and the Western Paleotethys paleobiogeographic realm. Furthermore, the width of the Paleotethys and Rheic oceans separating these regions is not considered excessive, particularly during the late Visean and early Serpukhovian.

The Design and Construction of Burton Bridge

1975 ◽  
Vol 2 (2) ◽  
pp. 209-240
Author(s):  
R. B. Malloy ◽  
D. J. Davies
Keyword(s):  
New Brunswick ◽  
The South ◽  
South Side ◽  
Arch Bridge ◽  
River Level ◽  
The North ◽  
North Bank ◽  
The One ◽  
Bridge Spans ◽  
The City

Burton Bridge spans the Saint John River about 14 miles (~22 km) downstream from the city of Fredericton, New Brunswick, replacing a ferry service between Maugerville on the Trans-Canada Highway along the north bank of the river, and the township of Burton on the south side of the river. The ferry service, said to have been in use for over two hundred years, met with increasing criticism in recent years and a demand for its replacement by a bridge has resulted in the present structure, completed and opened to traffic in the autumn of 1972. The main span is an arch bridge with a center navigation span of 600 ft (182.9 m), and an overall length of 1026.5 ft (312.9 m), flanked on each side by three 125 ft (38.1 m) approach spans. The total length of bridge between the abutments is 1784.5 ft (543.9 m), and its greatest height above normal river level in summer is 185 ft (56.4 m). Access to the bridge from the existing roads is accomplished by approach roads on new embankments, the one on the south side being relatively short, while those on the north bank form a complex of roads providing east and west access to the Trans-Canada Highway, over which a pre-stressed concrete overpass bridge has been built for one of the routes.

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