Sir William Dawson (1820–1899): a very modern paleobotanist

  title={Sir William Dawson (1820–1899): a very modern paleobotanist},
  author={H. Falcon-Lang and J. Calder},
  journal={Atlantic Geology},
Sir William Dawson was one of Canada’s 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 Dawson’s success was his recognition of the importance of a field-based research program, in which fossil plants could be observed in their precise… Expand
Marie Stopes and the Fern Ledges of Saint John, New Brunswick
Abstract Marie Stopes (1880–1958) is best known for her controversial writings on sex, marriage and birth control, but during her 20s and 30s she carved out a successful career as a palaeobotanist.Expand
The Pennsylvanian tropical biome reconstructed from the Joggins Formation of Nova Scotia, Canada
The Pennsylvanian (Langsettian) Joggins Formation contains a diverse fossil assemblage, first made famous by Lyell and Dawson in the mid-19th century. Collector curves based on c. 150 years ofExpand
The Joggins Fossil Cliffs UNESCO World Heritage site: a review of recent research
The Joggins Fossil Cliffs UNESCO World Heritage Site is a Carboniferous coastal section along the shores of the Cumberland Basin, an extension of Chignecto Bay, itself an arm of the Bay of Fundy,Expand
Catastrophically buried Middle Pennsylvanian Sigillaria and calamitean sphenopsids from Indiana, USA: What kind of vegetation was this?
Abstract A catastrophically buried stand of calamitean sphenopsids and sigillarian lycopsids is reported from the Middle Pennsylvanian of southwestern Indiana, in the Illinois Basin. The plants wereExpand
Chapter 6 The Maritimes Basin of Atlantic Canada: Basin Creation and Destruction in the Collisional Zone of Pangea
Abstract During the final assembly of Pangea, the Maritimes Basin of Atlantic Canada was tectonically active for ∼120 Myr from the Mid-Devonian to the Early Permian, following terrane accretion andExpand
From Scratch: Building the Governance Structure of the Joggins Fossil Institute
The Joggins Fossil Cliffs UNESCO World Heritage Site is managed by the Joggins Fossil Institute (JFI), a charitable organization consisting of a volunteer board of directors and a small staff team.Expand


On the Remains of a Reptile (Dendrerpeton Acadianum, Wyman and Owen) and of a Land Shell discovered in the Interior of an Erect Fossil Tree in the Coal Measures of Nova Scotia
Descriptions and sections of the Coal-formation of Nova Scotia, and particularly of the cliffs called the South Joggins, have been published by Messrs. Jackson and Alger*, Mr. Brown†, Dr. Gesner‡,Expand
A fossil lycopsid forest succession in the classic Joggins section of Nova Scotia: Paleoecology of a disturbance-prone Pennsylvanian wetland
Standing lycopsid trees occur at 60 or more horizons within the 1425 m thick coal-bearing interval of the classic Carboniferous section at Joggins, with one of the most consistently productiveExpand
Note on a Specimen of Diploxylon from the Coal-formation of Nova Scotia
  • J. Dawson
  • Geology
  • Quarterly Journal of the Geological Society of London
  • 1877
In a recent visit to the South Joggins, with the view of further studying the fossils of that district, and more especially of searching for reptilian remains in any erect stumps of Sigillaria thatExpand
On Fossil Plants from the Coal Formation of Cape Breton
  • C. J. F. Bunbary
  • Geology
  • Quarterly Journal of the Geological Society of London
  • 1847
Since Mr. Lyell gave, in his ‘Travels in North America,’ a catalogue of the fossil plants occurring in the coal formation of Nova Scotia, I have received, through the kindness of Richard Brown, Esq.,Expand
Lyell’s Principles of Geology: foundations of sedimentology
  • M. Leeder
  • Geology
  • Geological Society, London, Special Publications
  • 1998
Abstract This chapter examines the extensive arguments Lyell brought to bear on the interpretation of sedimentary rocks through the operation of ‘present causes’ in the first Edition of Principles ofExpand
Description of a peculiar Fossil Fern from the Sydney Coal Field, Cape Breton
  • C. J. F. Bunbury
  • Geology
  • Quarterly Journal of the Geological Society of London
  • 1852
The fossil plant of which I propose to give an account was communicated to me some time ago by Richard Brown, Esq., from the coalmines of Sydney, Cape Breton. I have shown it to several of my mostExpand
Upland ecology of some Late Carboniferous cordaitalean trees from Nova Scotia and England
Abstract Permineralised logs and charcoal fragments composed of Dadoxylon -type wood and derived from cordaitalean trees are described from the Upper Carboniferous (Westphalian) of Nova Scotia andExpand
Notices of some Fossils found in the Coal Formation of Nova Scotia
  • J. Dawson
  • Geology
  • Quarterly Journal of the Geological Society of London
  • 1846
Ichnolites.—The coal-formation of Nova Scotia has already yielded ichnolites of three species, specimens of which, all unfortunately very imperfect, have been presented to the Geological Societby Mr.Expand
On a Terrestrial Mollusk, a Chilognathous Myriapod, and some New Species of Reptiles, from the Coal-Formation of Nova Scotia
  • J. Dawson
  • Geology
  • Quarterly Journal of the Geological Society of London
  • 1860
On revisiting the South Joggins in the past summer, principally with the view of collecting material for the further prosecution of my researches on the structure of coal, I was informed by Mr.Expand
Notice of the Discovery of Additional Remains of Land Animals in the Coal-Measures of the South Joggins, Nova Scotia
  • J. Dawson
  • Geology
  • Quarterly Journal of the Geological Society of London
  • 1862
In the long range of rapidly wasting cliffs at the South Joggins, every successive year exposes new examples of erect trees and other fossils; and, as the removal of the fallen débris is equallyExpand