{"title":"An Early Cainozoic (Paleocene) foraminiferal fauna with Fabiania from offshore eastern Australia","authors":"P. Quilty, S. Shafik, C. Jenkins, J. Keene","doi":"10.1080/03115519708619170","DOIUrl":null,"url":null,"abstract":"Early Paleocene marine sediments are recorded from a single dredge sample taken from the continental slope (3533–3306 m) off the central coast of New South Wales. They probably belong to the Early Paleocene NP4 calcareous nannoplankton zone (P1c or P1d/P2 in standard formainiferal zonal terms) and thus are the first Palaeogene marine rocks known from the region and the first record of marine biota of this age from the Australian margin other than Western Australia. The age is based on analysis of calcareous nannofossils. The sediment accumulated in very shallow, warm, fully marine conditions, apparently off a coast of periodically low runoff, and the fauna lacks any planktonic foraminiferal species. While it is domainated by several typically Paleocene benthic forms well known from southern and southwestern Australia, several otherwise typical Australian forms appear to be absent. Fabiania (the new species F. macgowrani) is recorded for the first time from Australia, apparently the earliest known occurren...","PeriodicalId":50830,"journal":{"name":"Alcheringa","volume":"21 1","pages":"299-315"},"PeriodicalIF":1.2000,"publicationDate":"1997-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1080/03115519708619170","citationCount":"6","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Alcheringa","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1080/03115519708619170","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
引用次数: 6
Abstract
Early Paleocene marine sediments are recorded from a single dredge sample taken from the continental slope (3533–3306 m) off the central coast of New South Wales. They probably belong to the Early Paleocene NP4 calcareous nannoplankton zone (P1c or P1d/P2 in standard formainiferal zonal terms) and thus are the first Palaeogene marine rocks known from the region and the first record of marine biota of this age from the Australian margin other than Western Australia. The age is based on analysis of calcareous nannofossils. The sediment accumulated in very shallow, warm, fully marine conditions, apparently off a coast of periodically low runoff, and the fauna lacks any planktonic foraminiferal species. While it is domainated by several typically Paleocene benthic forms well known from southern and southwestern Australia, several otherwise typical Australian forms appear to be absent. Fabiania (the new species F. macgowrani) is recorded for the first time from Australia, apparently the earliest known occurren...
期刊介绍:
Alcheringa : An Australasian Journal of Palaeontology is the official journal of the Australasian Palaeontologists.
Alcheringa covers all aspects of palaeontology and its ramifications into the earth and biological sciences, including:
Taxonomy-
Biostratigraphy-
Micropalaeontology-
Vertebrate palaeontology-
Palaeobotany-
Palynology-
Palaeobiology-
Palaeoanatomy-
Palaeoecology-
Biostratinomy-
Biogeography-
Chronobiology-
Biogeochemistry-
Palichnology.
Review articles are welcome, and may be solicited from time to time. Thematic issues are also possible. Emphasis is placed on high quality and informative illustration, in both line drawings and photographs. Papers of general significance may receive preference over those of more local interest.