Diatoms (Bacillariophyta)

Abstract The diatoms are one of the most easily recognizable groups of major eukaryotic algae, because of their unique siliciAed cell walls (frustules), which consist of two overlapping thecae, each in turn consisting of a valve and a number of hooplike or segmental girdle bands (1). Well-preserved...

Full description

Bibliographic Details
Main Author: Medlin, Linda K
Format: Book Part
Language:English
Published: Oxford University PressOxford 2009
Subjects:
Antarc*
Antarctica
Weddell Sea
Online Access:http://dx.doi.org/10.1093/oso/9780199535033.003.0010
https://academic.oup.com/book/chapter-pdf/52373764/isbn-9780199535033-book-part-10.pdf
id croxfordunivpr:10.1093/oso/9780199535033.003.0010
record_format openpolar
spelling croxfordunivpr:10.1093/oso/9780199535033.003.0010 2024-09-15T17:45:16+00:00 Diatoms (Bacillariophyta) Medlin, Linda K 2009 http://dx.doi.org/10.1093/oso/9780199535033.003.0010 https://academic.oup.com/book/chapter-pdf/52373764/isbn-9780199535033-book-part-10.pdf en eng Oxford University PressOxford The Timetree of Life page 127-130 ISBN 9780199535033 9781383044720 book-chapter 2009 croxfordunivpr https://doi.org/10.1093/oso/9780199535033.003.0010 2024-08-19T04:24:12Z Abstract The diatoms are one of the most easily recognizable groups of major eukaryotic algae, because of their unique siliciAed cell walls (frustules), which consist of two overlapping thecae, each in turn consisting of a valve and a number of hooplike or segmental girdle bands (1). Well-preserved frustules are found in the earliest known deposits of fossil diatoms, from the early Albian (125 Ma) of what is now the Weddell Sea, Antarctica, but these diatoms bear no resemblance to modern diatoms in their morphology (2). Book Part Antarc* Antarctica Weddell Sea Oxford University Press 127 130
institution Open Polar
collection Oxford University Press
op_collection_id croxfordunivpr
language English
description Abstract The diatoms are one of the most easily recognizable groups of major eukaryotic algae, because of their unique siliciAed cell walls (frustules), which consist of two overlapping thecae, each in turn consisting of a valve and a number of hooplike or segmental girdle bands (1). Well-preserved frustules are found in the earliest known deposits of fossil diatoms, from the early Albian (125 Ma) of what is now the Weddell Sea, Antarctica, but these diatoms bear no resemblance to modern diatoms in their morphology (2).
format Book Part
author Medlin, Linda K
spellingShingle Medlin, Linda K
Diatoms (Bacillariophyta)
author_facet Medlin, Linda K
author_sort Medlin, Linda K
title Diatoms (Bacillariophyta)
title_short Diatoms (Bacillariophyta)
title_full Diatoms (Bacillariophyta)
title_fullStr Diatoms (Bacillariophyta)
title_full_unstemmed Diatoms (Bacillariophyta)
title_sort diatoms (bacillariophyta)
publisher Oxford University PressOxford
publishDate 2009
url http://dx.doi.org/10.1093/oso/9780199535033.003.0010
https://academic.oup.com/book/chapter-pdf/52373764/isbn-9780199535033-book-part-10.pdf
genre Antarc*
Antarctica
Weddell Sea
genre_facet Antarc*
Antarctica
Weddell Sea
op_source The Timetree of Life
page 127-130
ISBN 9780199535033 9781383044720
op_doi https://doi.org/10.1093/oso/9780199535033.003.0010
container_start_page 127
op_container_end_page 130
_version_ 1810493018145292288

Similar Items