An Early Jurassic flora from the Clarence-Moreton Basin, Australia
(2008) In Review of Palaeobotany and Palynology 150(1-4). p.5-21- Abstract
- A low-diversity Early Jurassic flora preserved in floodbasin siltstones of the Marburg Subgroup at Inverleigh Quarry in the Clarence-Moreton Basin, eastern Australia, is dominated by Allocladus helgei Jansson sp. nov., a conifer with denticulate leaves tentatively attributed to Araucariaceae. The assemblage also includes Rintoulia variabilis and Caytoniales, (Caytonia cucullata McLoughlin sp. nov. and cf. Sagenopteris nilssoniana), reinforcing the wide distribution of this order in Early to Middle Jurassic floras of Gondwana. Ferns (Cladophlebis and Sphenopteris species) and isoetalean lycophytes (Isoetites sp.) constitute the herbaceous elements of the flora. The palynoflora is dominated by cheirolepidiacean (Classopollis) pollen and is... (More)
- A low-diversity Early Jurassic flora preserved in floodbasin siltstones of the Marburg Subgroup at Inverleigh Quarry in the Clarence-Moreton Basin, eastern Australia, is dominated by Allocladus helgei Jansson sp. nov., a conifer with denticulate leaves tentatively attributed to Araucariaceae. The assemblage also includes Rintoulia variabilis and Caytoniales, (Caytonia cucullata McLoughlin sp. nov. and cf. Sagenopteris nilssoniana), reinforcing the wide distribution of this order in Early to Middle Jurassic floras of Gondwana. Ferns (Cladophlebis and Sphenopteris species) and isoetalean lycophytes (Isoetites sp.) constitute the herbaceous elements of the flora. The palynoflora is dominated by cheirolepidiacean (Classopollis) pollen and is attributable to the upper part of the Corollina (=Classopollis) torosa Zone of late Pliensbachian-early Toarcian age (180-185 Ma). The Inverleigh flora represents one of the few Australian assemblages dated between the major phases of floristic turnover at the end of the Triassic and the Toarcian. Sedimentological characteristics, cuticular features of the conifer leaves and the abundance of free-sporing plants indicate a relatively humid palaeoclimate for the Clarence-Moreton Basin Early Jurassic. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/939640
- author
- Jansson, Ida-Maria ; McLoughlin, Stephen ; Vajda, Vivi LU and Pole, Michael
- organization
- publishing date
- 2008
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Review of Palaeobotany and Palynology
- volume
- 150
- issue
- 1-4
- pages
- 5 - 21
- publisher
- Elsevier
- external identifiers
-
- wos:000257037500002
- scopus:43849104354
- ISSN
- 0034-6667
- DOI
- 10.1016/j.revpalbo.2008.01.002
- language
- English
- LU publication?
- yes
- id
- 69cc8de7-03ab-41ec-9b14-8d9e84bae9e3 (old id 939640)
- date added to LUP
- 2016-04-01 13:21:24
- date last changed
- 2022-03-06 05:26:19
@article{69cc8de7-03ab-41ec-9b14-8d9e84bae9e3, abstract = {{A low-diversity Early Jurassic flora preserved in floodbasin siltstones of the Marburg Subgroup at Inverleigh Quarry in the Clarence-Moreton Basin, eastern Australia, is dominated by Allocladus helgei Jansson sp. nov., a conifer with denticulate leaves tentatively attributed to Araucariaceae. The assemblage also includes Rintoulia variabilis and Caytoniales, (Caytonia cucullata McLoughlin sp. nov. and cf. Sagenopteris nilssoniana), reinforcing the wide distribution of this order in Early to Middle Jurassic floras of Gondwana. Ferns (Cladophlebis and Sphenopteris species) and isoetalean lycophytes (Isoetites sp.) constitute the herbaceous elements of the flora. The palynoflora is dominated by cheirolepidiacean (Classopollis) pollen and is attributable to the upper part of the Corollina (=Classopollis) torosa Zone of late Pliensbachian-early Toarcian age (180-185 Ma). The Inverleigh flora represents one of the few Australian assemblages dated between the major phases of floristic turnover at the end of the Triassic and the Toarcian. Sedimentological characteristics, cuticular features of the conifer leaves and the abundance of free-sporing plants indicate a relatively humid palaeoclimate for the Clarence-Moreton Basin Early Jurassic.}}, author = {{Jansson, Ida-Maria and McLoughlin, Stephen and Vajda, Vivi and Pole, Michael}}, issn = {{0034-6667}}, language = {{eng}}, number = {{1-4}}, pages = {{5--21}}, publisher = {{Elsevier}}, series = {{Review of Palaeobotany and Palynology}}, title = {{An Early Jurassic flora from the Clarence-Moreton Basin, Australia}}, url = {{http://dx.doi.org/10.1016/j.revpalbo.2008.01.002}}, doi = {{10.1016/j.revpalbo.2008.01.002}}, volume = {{150}}, year = {{2008}}, }