148 research outputs found
Earliest history of coal mining and grindstone quarrying at Joggins, Nova Scotia, and its implications for the meaning of the place name âJogginsâ
The rich history of coal mining and grindstone quarrying at Joggins, Nova Scotia, prior to Lyellâs visit in 1842 is less well known than its subsequent history. Franquelin first observed coal there in 1686, and within little more than a decade Acadian coal mines had sprung up at the Coal Cliffs. Following the British acquisition of Nova Scotia in 1713, the coal mines attracted Captain Belcher and other New England traders, who loaded their ships with coal for sale in Boston. In 1731, eager to impose duty on this unregulated trade, the Nova Scotia Council sponsored a British coal mine at Joggins operated by Major Cope. Unable to safely load ships at the Coal Cliffs, Cope constructed a wharf and coal depot at Granâchoggin (present-day Downing Cove), seven miles to the north of the mine. It was by association with this depot that the Coal Cliffs later became known as Joggins. Copeâs coal mine survived less than eighteen months before the Miâkmaq, aided and abetted by Acadians, destroyed the site in 1732. Following this episode, Acadians worked the Joggins coal mines until they fell under the control of British forces engaged in the Seven Years War in 1756. Subsequently, the Lords of Trade suppressed coal mining at Joggins, fearing it would harm British imports, and full-scale operations did not recommence until 1847. During this lull, the grindstone industry boomed. Beginning sometime before 1764, the principal stone quarries operated at Lower Cove, where the famous Blue-Grit was cut. Grindstone quarries were also worked on the Maringouin Peninsula and the two opposing sides of Chignecto Bay became known as the North and South Joggins.
RĂSUMĂ
On connaĂźt moins bien le riche passĂ© de lâextraction du charbon et de la pierre meuliĂšre Ă Joggins, NouvelleâĂcosse, avant la visite de Lyell en 1842, que son passĂ© subsĂ©quent. Franquelin y avait observĂ© du charbon pour la premiĂšre fois en 1686 et en lâespace dâun peu plus dâune dĂ©cennie, plusieurs mines de charbon acadiennes Ă©taient apparues Ă Coal Cliffs. Ă la suite de lâacquisition de la NouvelleâĂcosse par les Britanniques en 1713, les mines de charbon ont attirĂ© le capitaine Belcher et dâautres commerçants de la NouvelleâAngleterre qui chargeaient leurs vaisseaux de charbon pour le vendre Ă Boston. En 1731, impatient dâimposer des droits sur ce commerce non rĂ©glementĂ©, le Conseil de la NouvelleâĂcosse a parrainĂ© lâexploitation Ă Joggins dâune mine de charbon britannique exploitĂ©e par le major Cope. Incapable de charger de façon sĂ©curitaire les navires Ă Coal Cliffs, Cope construisit un quai et un dĂ©pĂŽt de charbon Ă Granâchoggin (anse Downing actuelle), Ă sept milles au nord de la mine. Lâassociation Ă ce dĂ©pĂŽt a plus tard confĂ©rĂ© Ă Coal Cliffs le nom de Joggins. La mine de charbon de Cope a subsistĂ© moins de 18 mois jusquâĂ ce que les Micmacs, aidĂ©s et soutenus par les Acadiens, dĂ©truisirent lâemplacement en 1732. AprĂšs cet Ă©pisode, les Acadiens ont exploitĂ© les mines de charbon de Joggins jusquâĂ ce quâelles tombent sous le contrĂŽle des forces britanniques engagĂ©es dans la guerre de Sept Ans en 1756. Les lords du commerce ont subsĂ©quemment supprimĂ© lâextraction du charbon Ă Joggins, par crainte quâelle fasse tort aux importations britanniques, et lâexploitation Ă grande Ă©chelle nâa pas recommencĂ© avant 1847. Pendant cette pĂ©riode dâaccalmie, lâindustrie de la pierre meuliĂšre a connu un essor notable. Les principales carriĂšres de pierre ont commencĂ© leurs activitĂ©s dans les annĂ©es ayant prĂ©cĂ©dĂ© 1764 Ă Lower Cove, oĂč lâon extrayait le fameux grĂšs dur bleu. Des carriĂšres de pierre meule ont Ă©galement Ă©tĂ© exploitĂ©es sur la pĂ©ninsule Maringouin et les deux rives opposĂ©es de la baie Chignectou devinrent connues sous les noms de North et South Joggins
Anatomically-preserved cordaitalean trees from Lower Pennsylvanian (Langsettian) dryland alluvial-plain deposits at Joggins, Nova Scotia
Recent discoveries at Joggins, Nova Scotia have altered our understanding of the Pennsylvanian tropical biome. Of particular signiïŹcance has been the recognition of seasonal dryland ecosystems, compositionally distinct from the peat-forming wetland rainforests. Here I describe two anatomically-preserved fossil plant specimens from dryland alluvial plain facies. The ïŹrst specimen, Mesoxylon cf. sutclifïŹ i, is previously unknown from Joggins. It is a septate cordaitalean axis with mesarch leaf traces and a non-sympodial vasculature. Where found as isolated blocks, the secondary xylem of this plant has previously been classiïŹed as Dadoxylon recentium. The axis exhibits subtle growth interruptions suggestive of tropical rainfall seasonality, while associated traumatic zones may record ïŹre-damage. The second specimen is a Dadoxylon stump rooted within well-drained ïŹoodbasin soils. It conïŹrms earlier conjecture, based on parautochthonous assemblages, that cordaitalean trees grew in inter-channel areas. Together these new specimens improve our knowledge of the composition and ecology of seasonal dryland vegetation at Joggins.
RĂSUMĂ
Des dĂ©couvertes rĂ©centes Ă Joggins (Nouvelle-Ăcosse), ont modiïŹĂ© notre comprĂ©hension du biome tropical pennsylvanien. La reconnaissance d'Ă©cosystĂšmes de milieux arides saisonniers aux compositions distinctes des forĂȘts tropicales humides ayant formĂ© des tourbiĂšres, s'avĂšre particuliĂšrement importante. Je dĂ©cris aux prĂ©sentes deux spĂ©cimens prĂ©servĂ©s de plantes fossiles anatomiquement provenant du faciĂšs d'une plaine alluviale de milieu aride. Le premier spĂ©cimen, un Mesoxylon cf. sutclifïŹ i, Ă©tait auparavant inconnu Ă Joggins. Il s'agit d'un axe cordaitalĂ©en cloisonnĂ© comportant des cicatrices foliaires Ă arc moyen et une vasculature non sympodiale. Lors de sa dĂ©couverte sous forme de blocs isolĂ©s, on avait prĂ©cĂ©demment classiïŹĂ© le xylĂšme secondaire de cette plante en tant que Dadoxylon recentium L'axe prĂ©sente des interruptions de croissance subtiles Ă©voquant des chutes de pluie tropicales saisonniĂšres, tandis que les cernes traumatiques associĂ©s pourraient tĂ©moigner de dommages causĂ©s par le feu. Le second spĂ©cimen est une souche de Dadoxylon qui plongeait ses racines Ă l'intĂ©rieur des sols d'un bassin de crue bien drainĂ©. Il conïŹrme une conjecture antĂ©rieure, basĂ©e sur des assemblages parautochtones, supposant que les arbres cordaitalĂ©ens aient poussĂ© dans des secteurs situĂ©s entre des chenaux. Ces deux nouveaux spĂ©cimens amĂ©liorent notre connaissance de la composition et de l'Ă©cologie de la vĂ©gĂ©tation saisonniĂšre des milieux arides Ă Joggins.
[Traduit par la rédaction.
New Brunswick and Nova Scotia: the First Geological Field Trip by a North American College
The first known geological excursion by a North American college was conducted in 1835. Twenty staff and students belonging to Williams College â a liberal arts college in Massachusetts, USA â explored the geology bordering the Bay of Fundy in northeast Maine, New Brunswick and Nova Scotia. Led by two young professors of natural history, Ebenezer Emmons and Albert Hopkins, the party made extensive observations around Pasammaquoddy Bay, Saint John, Parrsboro, and Windsor, as well as more widely through the Minas and Cumberland basins. Although partly following in the footsteps of two pioneering Bostonians, Charles Jackson and Francis Alger, who had reconnoitred the region in the late 1820s, the Williams College party nevertheless made several original observations. One of most important was a study of the anatomy and paleoclimatic significance of permineralized plants from Joggins and Grindstone Island undertaken by Emmons. This was only the second study of its kind worldwide and later inspired William Dawson to do similar work. Largely overlooked by historians of geology, the Williams College expedition, which comprised a four-week voyage of about 1800 km, illustrates well the challenges and opportunities of geological field work in the early Nineteenth Century.
RĂSUMĂ
La premiĂšre excursion gĂ©ologique connue dâun collĂšge nordâamĂ©ricain a Ă©tĂ© rĂ©alisĂ©e en 1835. Vingt membres du personnel et Ă©tudiants du CollĂšge Williams â collĂšge dâarts libĂ©raux du Massachusetts, Etats-Unis â ont explorĂ© la gĂ©ologie des bords de la baie de Fundy dans le nordâest du Maine, au NouveauâBrunswick et en NouvelleâĂcosse. Le groupe dirigĂ© par deux jeunes professeurs dâhistoire naturelle, Ebenezer Emmons et Albert Hopkins, a effectuĂ© de nombreuses observations dans les environs de la baie de Passamaquoddy, de SaintâJean, de Parrsboro et de Windsor, ainsi que dans des secteurs plus Ă©tendus Ă lâintĂ©rieur des bassins Minas et Cumberland. MĂȘme si le groupe du CollĂšge Williams a en partie suivi les pas de deux pionniers de Boston, Charles Jackson et Francis Alger, qui avaient effectuĂ© une reconnaissance de la rĂ©gion vers la fin des annĂ©es 1820, il a nĂ©anmoins fait plusieurs observations originales. Lâune des plus importantes a Ă©tĂ© lâĂ©tude de lâanatomie et de lâimportance palĂ©oclimatique des vĂ©gĂ©taux minĂ©ralisĂ©s de Joggins et de lâĂźle Grindstone rĂ©alisĂ©e par Emmons. Il sâagissait seulement de la deuxiĂšme Ă©tude du genre Ă lâĂ©chelle mondiale; elle a ultĂ©rieurement inspirĂ© Williams Dawson Ă exĂ©cuter des travaux similaires. Largement nĂ©gligĂ©e par les historiens de gĂ©ologie, lâexpĂ©dition du CollĂšge Williams, qui a comportĂ© un voyage de quatre semaines dâenviron 1 800 kilomĂštres, illustre bien les dĂ©fis et les possibilitĂ©s qui sâoffraient dans le domaine des travaux gĂ©ologiques sur le terrain au dĂ©but du 19e siĂšcle. [Traduit par la redaction
A Cordaixylon axis from well-drained alluvial plain facies in the Lower Pennsylvanian Joggins Formation of Nova Scotia
Plant remains showing preservation of cellular anatomy are rare in the Lower Pennsylvanian Joggins Formation of Nova Scotia. Here I report an anatomically preserved cordaitalean axis that shows endarch maturation and a sympodial vascular architecture. The specimen belongs to the morphogenus Cordaixylon, but in the absence of extraxylary tissue or attached fertile material, it cannot be assigned to a species. Together with a previously reported Mesoxylon axis with mesarch and non-sympodial vasculature, the new discovery demonstrates the existence of both major organizational types of cordaitalean at this locality. Previous reports have identified Cordaixylon as a plant that preferred peat mire environments. In this paper, the morphogenus is recorded from well-drained alluvial plain facies, thus extending knowledge of its ecological range.
Résumé
Les vestiges de plantes prĂ©sentant une prĂ©servation de lâanatomie cellulaire sont rares Ă lâintĂ©rieur de la Formation du Pennsylvanien infĂ©rieur de Joggins, en Nouvelle-Ăcosse. Je fais part dans les prĂ©sentes dâun axe de cordaitalĂ©en natomiquement prĂ©servĂ© qui affiche une maturation circulaire Ă partir de lâintĂ©rieur et une architecture vasculaire sympodiale. Le spĂ©cimen fait partie du morphogenre Cordaixylon, mais en lâabsence de tissu extraxylaire ou de matiĂšre fertile y Ă©tant fixĂ©e, on ne peut pas le rattacher Ă une espĂšce donnĂ©e. La nouvelle dĂ©couverte, conjuguĂ©e Ă un axe de Mesoxylon prĂ©cĂ©demment signalĂ© qui comportait une vasculature non sympodiale Ă Ă©lĂ©ments en spirale internes, rĂ©vĂšle lâexistence des deux principaux types structuraux de cordaitalĂ©ens Ă cet emplacement. Des rapports antĂ©rieurs avaient dĂ©fini le Cordaixylon en tant que plante prĂ©fĂ©rant les environnements Ă bourbiers de tourbe. Le prĂ©sent document fait Ă©tat de lâobservation du morphogenre dâun faciĂšs de plaine alluviale bien drainĂ©e, ce qui Ă©tend notre connaissance de son aire de distribution Ă©cologique
Sir William Dawson (1820â1899): a very modern paleobotanist
Sir William Dawson was one of Canadaâs most influential Nineteenth Century geologists. Although a lifelong opponent of the concept of evolution, a stance that resulted in him being sidelined by the scientific community, he made enormous contributions to Pennsylvanian paleobotany, especially at the Joggins fossil cliffs of Nova Scotia. Key to Dawsonâs success was his recognition of the importance of a field-based research program, in which fossil plants could be observed in their precise geological context over a sustained period of time. Uniquely trained as both geologist and botanist, he was skilled in the microscopic analysis of permineralized plant anatomy, and appreciated the enormous potential of fossil charcoal as an untapped source of systematic information. Arguably his most extraordinary insights came in the field of plant taphonomy, in which studies of modern sedimentary processes and environments were used to interpret the rock record. His analysis of fossil plants in their sedimentary context allowed Pennsylvanian coal swamp communities, dominated by lycopsids and calamiteans, to be distinguished from the coniferopsid forests, which occupied mountainous regions further inland. The lasting significance of Dawsonâs paleobotanical work is emphasized by many recent papers concerning the Pennsylvanian coal measures of Atlantic Canada, which have either directly built on research topics that Dawson initiated, or have confirmed hypotheses that Dawson framed. Until recent times, the discipline of paleobotany has been dominated by systematic fossil plant description with little or no reference to geological context. By virtue of his distinctively holistic approach, synthesizing all available geological and botanical data, Dawson is marked out from his contemporaries. His methodology does not appear old-fashioned even today, and it is therefore with justification that we describe him as a very modern paleobotanist.
Resumé
Sir William Dawson a Ă©tĂ© lâun des gĂ©ologues les plus influents du 19e siĂšcle au Canada. MĂȘme sâil sâest opposĂ© toute sa vie au concept de lâĂ©volution, une position qui a amenĂ© le milieu scientifique Ă lâignorer, il a Ă©normĂ©ment contribuĂ© Ă la palĂ©obotanique pennsylvanienne, spĂ©cialement dans les falaises fossilifĂšres de Joggins de la Nouvelle-Ăcosse. La clĂ© du succĂšs de Dawson rĂ©side dans le fait quâil avait reconnu lâimportance dâun programme de recherche sur le terrain prĂ©voyant lâobservation des plantes fossiles dans leur milieu gĂ©ologique particulier pendant une pĂ©riode de temps prolongĂ©e. GrĂące Ă sa formation unique de gĂ©ologue et de botaniste, il possĂ©dait la compĂ©tence voulue pour rĂ©aliser une analyse microscopique de lâanatomie des plantes perminĂ©ralisĂ©es et il comprenait le potentiel Ă©norme du charbon de bois fossile comme source inexploitĂ©e de donnĂ©es systĂ©matiques. On pourrait soutenir que ses idĂ©es les plus extraordinaires se sont manifestĂ©es dans le domaine de la taphonomie vĂ©gĂ©tale, dans lequel des Ă©tudes dâenvironnements et de processus sĂ©dimentaires modernes ont servi Ă interprĂ©ter des antĂ©cĂ©dents lithologiques. Ses analyses de plantes fossiles dans leur contexte sĂ©dimentaire ont permis de distinguer les communautĂ©s des marĂ©cages houillers pennsylvaniens, dans lesquels prĂ©dominent les lycopsides et les calamites, des forĂȘts conifĂ©ropsides, qui occupaient les rĂ©gions montagneuses plus Ă lâintĂ©rieur des terres. De nombreuses communications rĂ©centes au sujet des couches houillĂšres pennsylvaniennes des provinces de lâAtlantique, qui sâappuient directement sur des sujets de recherches amorcĂ©es par Dawson ou ayant confirmĂ© des hypothĂšses formulĂ©es par Dawson, mettent en relief lâimportance durable des travaux palĂ©obotaniques de Dawson. La discipline de la palĂ©obotanique a jusquâĂ tout rĂ©cemment Ă©tĂ© dominĂ©e par des descriptions systĂ©matiques de plantes fossiles Ă©voquant Ă peine ou nâĂ©voquant pas du tout le contexte gĂ©ologique. Dawson sâest dĂ©marquĂ© de ses contemporains au moyen de son approche nettement holistique en rĂ©alisant une synthĂšse de toutes les donnĂ©es gĂ©ologiques et botaniques accessibles. Sa mĂ©thode de travail ne semble pas rĂ©trograde, mĂȘme aujourdâhui, et il est par consĂ©quent tout Ă fait justifiĂ© que nous le dĂ©crivions en tant que palĂ©obotaniste trĂšs moderne
A new Upper Cretaceous ginkgoalean reproductive structure Nehvizdyella from the Czech Republic and its whole-plant reconstruction
Uplands, lowlands, and climate:Taphonomic megabiases and the apparent rise of a xeromorphic, drought-tolerant flora during the Pennsylvanian-Permian transition
Stratigraphy and sedimentology of early Pennsylvanian red beds at Lower Cove, Nova Scotia, Canada: the Little River Formation with redefinition of the Joggins Formation
The coastal cliffs along the eastern shore of Chignecto Bay, Nova Scotia contain one of the finest Carboniferous sections in the world. In 1843, Sir William Logan measured the entire section as the first project of the Geological Survey of Canada, and defined eight stratigraphic divisions. We have re-measured a section corresponding almost exactly with Loganâs Division 5 in bed-by-bed detail. The strata are exposed in the wave-cut platform and low-relief bluffs of a 2 km-long section at Lower Cove, near Joggins, north and south of Little River. This 635.8 metre-thick succession until now has been included within the basal part of the Joggins Formation, and overlies the Boss Point Formation. However, the studied strata are lithologically distinct, and are formally recognized as the new Little River Formation. This formation is bounded by regionally important surfaces and is traceable inland for 30 kilometres from its Lower Cove type section. Facies analysis indicates that it represents the deposits of a well-drained alluvial plain dissected by shallow rivers characterized by flashy flow. It can be clearly distinguished from the underlying Boss Point Formation (Loganâs Division 6) by its much smaller channels, and from the overlying Joggins Formation (Loganâs Division 4) by lack of coal seams and bivalve-bearing limestone beds. Palynological assemblages indicate that the Little River Formation is of probable late Namurian to basal Westphalian (basal Langsettian) age, and is a likely time-equivalent of the informal Grand-Anse formation of southeast New Brunswick.
Resumé
Les falaises cĂŽtiĂšres longeant le rivage oriental de la baie Chignectou, en Nouvelle-Ăcosse, abritent lâun des stratotypes carbonifĂšres les plus intĂ©ressants dans le monde. Sir William Logan avait mesurĂ© en 1843 lâensemble du stratotype dans le cadre du premier projet de la Commission gĂ©ologique du Canada et il avait dĂ©fini huit divisions stratigraphiques. Nous avons mesurĂ© Ă nouveau un stratotype correspondant presque exactement dans ses dĂ©tails couche par couche Ă la division 5 de Logan. Les strates affleurent dans une plate-forme dâĂ©rosion et des falaises de relief Ă©moussĂ© dâun secteur de deux kilomĂštres de longueur Ă lâanse Lower, prĂšs de Joggins, au nord et au sud de la riviĂšre Little. Cette succession de 635,8 mĂštres dâĂ©paisseur avait jusquâĂ maintenant Ă©tĂ© incluse Ă lâintĂ©rieur de la partie basale de la Formation de Joggins et elle recouvre la Formation de Boss Point. Les strates Ă©tudiĂ©es sont cependant lithologiquement distinctes et on les reconnaĂźt officiellement en tant que nouvelle Formation de Little River. Cette formation est limitĂ©e par des surfaces importantes Ă lâĂ©chelle rĂ©gionale; on peut la retracer Ă lâintĂ©rieur des terres sur 30 kilomĂštres Ă partir de son stratotype de lâanse Lower. Une analyse du faciĂšs rĂ©vĂšle quâil reprĂ©sente les dĂ©pĂŽts dâune plaine alluviale bien drainĂ©e, sectionnĂ©e par des riviĂšres peu profondes caractĂ©risĂ©es par des crues Ă©clair. On peut nettement la distinguer de la Formation sous-jacente de Boss Point (division 6 de Logan), grĂące Ă ses canaux beaucoup plus petits, ainsi que de la Formation sus-jacente de Joggins (division 4 de Logan), par lâabsence de couches houillĂšres et de couches de calcaire abritant des
lamellibranches. Les assemblages palynologiques rĂ©vĂšlent que la Formation de Little River remonte probablement Ă la pĂ©riode du Namurien tardif au Westphalien basal (Langsettien basal) et quâelle constitue vraisemblablement un Ă©quivalent chronologique de la Formation officieuse de Grande-Anse dans le sud-est du Nouveau-Brunswick
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