SILURIAN SPORES AND CRYPTOSPORES FROM THE ARISAIG GROUP, NOVA SCOTIA, CANADA
Bibliographic record
Abstract
Research Article| January 01, 2001 SILURIAN SPORES AND CRYPTOSPORES FROM THE ARISAIG GROUP, NOVA SCOTIA, CANADA JOHN H. BECK; JOHN H. BECK Weston Observatory Paleobotany Laboratory, 381 Concord Road, Weston, MA 02193, U.S.A. Search for other works by this author on: GSW Google Scholar PAUL K. STROTHER PAUL K. STROTHER Weston Observatory Paleobotany Laboratory, 381 Concord Road, Weston, MA 02193, U.S.A. Search for other works by this author on: GSW Google Scholar Palynology (2001) 25 (1): 127–177. https://doi.org/10.2113/0250127 Article history first online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation JOHN H. BECK, PAUL K. STROTHER; SILURIAN SPORES AND CRYPTOSPORES FROM THE ARISAIG GROUP, NOVA SCOTIA, CANADA. Palynology 2001;; 25 (1): 127–177. doi: https://doi.org/10.2113/0250127 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search nav search search input Search input auto suggest search filter All ContentBy SocietyPalynology Search Advanced Search Abstract The Arisaig Group in northern mainland Nova Scotia has the most complete sequence of Silurian, fine grained, siliciclastic, near-shore marine sediments in Western Avalonia. In this setting, the Arisaig Group received a nearly continuous supply of autochthonous marine and allochthonous nonmarine palynomorphs. One hundred and seventy-seven samples, ranging in age from latest Ordovician?–early Llandovery to Přídolí (Beechhill Cove to Stonehouse formations) yield the most diverse spore assemblage yet known from the Silurian of North America. This paper describes the spores and cryptospores and reexamines age relationships of the Arisaig Group, placing both within context of early land plant evolution.Thirty-six species of spores and cryptospores were found in the Arisaig Group. Six new species are Ambitisporites marginatus sp. nov., A. capitaneus sp. nov., Scylaspora asperverruca sp. nov., Chelinospora textilis sp. nov., Hispanaediscus scabiosus sp. nov., and Hispanaediscus imbricatus sp. nov. A new genus, Vermiverruspora is created and the original description of ChelinosporaAllen 1965 is resurrected. Six species of Chelinospora are reassigned to Vermiverruspora gen. nov. (C. paravermiculata Loboziak et al. 1988, C. vermiculata Chaloner & Streel 1968, C. ?vermiculataMcGregor & Camfield 1976, C. retorrida Turnau 1986, C. rumneyiBurgess & Richardson 1995, C. vermolutaBurgess & Richardson 1995) and one species transferred to Stellatispora (pattersoniiWellman 1993). Four additional sporomorphs believed to be new, are not formally named because better preserved specimens are needed.The Arisaig Group (West Avalonia) is similar to sporomorph-rich type sections in the Anglo-Welsh Basin (East Avalonia). Four assemblage zones (avitus–dilutus, brevicosta–verrucatus, libycus–poecilomorphus, and tripapillatus–spicula), and four assemblage sub-zones (A. brevicosta, E. protophanus, C. obscura, and S. inframurinata var. inframurinata) have been recognized. Sporomorphs indicate that the contacts between the Lower and Upper Members of the McAdam Brook Formation and Green Member of the Moydart Formation may be one to two graptolite biozones older than previously reported.The Arisaig palynomorphs support the theory that a major radiation of vascular land plants occurred during the latter half of the Silurian Period. Llandovery and early Wenlock deposits at Arisaig contain only a few species of smooth walled spores and cryptospores. Sixteen trilete spore and fifteen cryptospore species appear between the Homerian and the late Přídolí. The tempo and composition of this diversification reflect evolutionary events observed elsewhere in the world. You do not currently have access to this article.
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.001 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.004 | 0.006 |
| Science and technology studies | 0.003 | 0.001 |
| Scholarly communication | 0.001 | 0.000 |
| Open science | 0.001 | 0.001 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.011 | 0.002 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".