Circumboreal diatom Navicula streckerae Lange-Bert. & Witk., especially on lineolae
Navicula streckerae was recorded in two locations of northern Germany and the Arctic Ocean. According to the findings of this taxon from Lake Khovsgol (Mongolia) and Kamchatka (Russia) by our investigations, this taxon distributed northward from latitude 50°N. on the Eurassian Continent and is consi...
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National Institute of Polar Research
2012-11-01
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Series: | Antarctic Record |
Online Access: | http://doi.org/10.15094/00009662 |
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doaj-a418e99fd82b4dd6bc3ca20aed1390fb2020-11-24T22:06:33ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X2012-11-0156325928310.15094/00009662Circumboreal diatom Navicula streckerae Lange-Bert. & Witk., especially on lineolaeHiroshi Fukushima0Tsutomu Kimura1Tsuyako Ko-Bayashi2Sakiko Yoshitake3E.V. Lepskaya4Institute of PhycologyInstitute of PhycologyInstitute of PhycologyGuest Professor of Shonan Junior CollegeInstitute for Fisheries Research and OceanogaphyNavicula streckerae was recorded in two locations of northern Germany and the Arctic Ocean. According to the findings of this taxon from Lake Khovsgol (Mongolia) and Kamchatka (Russia) by our investigations, this taxon distributed northward from latitude 50°N. on the Eurassian Continent and is considered to be a circumboreal diatom. This taxon is divided into three types, namely the Arctic Ocean type, the Weser River type and the Kinzig River type according to the valve morphology. In this study we compare these three types in the samples from Europe and Kamchatka focusing on the valve form and sizes. Though the density of lineolae composing striae is one of the important characteristics to classify the species, there are few records of this point. We investigate this point in detail in the specimens from Europe and Kamchatka. Consequentry the two extreme values, short striae forming the cental area and the area including Voigt discontinuities, should be excluded when measuring the density of lineolae to obtain a stable value.http://doi.org/10.15094/00009662 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Hiroshi Fukushima Tsutomu Kimura Tsuyako Ko-Bayashi Sakiko Yoshitake E.V. Lepskaya |
spellingShingle |
Hiroshi Fukushima Tsutomu Kimura Tsuyako Ko-Bayashi Sakiko Yoshitake E.V. Lepskaya Circumboreal diatom Navicula streckerae Lange-Bert. & Witk., especially on lineolae Antarctic Record |
author_facet |
Hiroshi Fukushima Tsutomu Kimura Tsuyako Ko-Bayashi Sakiko Yoshitake E.V. Lepskaya |
author_sort |
Hiroshi Fukushima |
title |
Circumboreal diatom Navicula streckerae Lange-Bert. & Witk., especially on lineolae |
title_short |
Circumboreal diatom Navicula streckerae Lange-Bert. & Witk., especially on lineolae |
title_full |
Circumboreal diatom Navicula streckerae Lange-Bert. & Witk., especially on lineolae |
title_fullStr |
Circumboreal diatom Navicula streckerae Lange-Bert. & Witk., especially on lineolae |
title_full_unstemmed |
Circumboreal diatom Navicula streckerae Lange-Bert. & Witk., especially on lineolae |
title_sort |
circumboreal diatom navicula streckerae lange-bert. & witk., especially on lineolae |
publisher |
National Institute of Polar Research |
series |
Antarctic Record |
issn |
0085-7289 2432-079X |
publishDate |
2012-11-01 |
description |
Navicula streckerae was recorded in two locations of northern Germany and the Arctic Ocean. According to the findings of this taxon from Lake Khovsgol (Mongolia) and Kamchatka (Russia) by our investigations, this taxon distributed northward from latitude 50°N. on the Eurassian Continent and is considered to be a circumboreal diatom. This taxon is divided into three types, namely the Arctic Ocean type, the Weser River type and the Kinzig River type according to the valve morphology. In this study we compare these three types in the samples from Europe and Kamchatka focusing on the valve form and sizes. Though the density of lineolae composing striae is one of the important characteristics to classify the species, there are few records of this point. We investigate this point in detail in the specimens from Europe and Kamchatka. Consequentry the two extreme values, short striae forming the cental area and the area including Voigt discontinuities, should be excluded when measuring the density of lineolae to obtain a stable value. |
url |
http://doi.org/10.15094/00009662 |
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