Abstract
SINCE contributing the chapter in the history of the Coniferæ upon which Prof. Haughton remarks, I have seen Araucaria Cunninghami growing in gardens round Funchal, and my belief in the specific identity of the Bournemouth Eocene plant is further strengthened; yet still, as only foliage is known in the fossil, I should hardly be prepared to contest upon that alone a question of climate, however minute the resemblance. But even with the most undisputed identity there are so many possibilities of error in arguing from a single species, that little importance should be attached to conclusions drawn from it.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
Rights and permissions
About this article
Cite this article
GARDNER, J. Geological Climates. Nature 23, 53–54 (1880). https://doi.org/10.1038/023053d0
Issue date:
DOI: https://doi.org/10.1038/023053d0