ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ

P(論文) The Kasumi Rock Ice-Free Area is located at 68°21'5"1.S. and 42°15'13"1.E. This area seems to have experienced not so many years since the glacial epoch, as no evidence of weathering nor weathered rocks were found there. Moss and lichen were not seen either. Only moraines w...

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Bibliographic Details
Main Authors: 福島, 博, フクシマ, ヒロシ, FUKUSHIMA, Hiroshi
Language:Japanese
Published: 国立極地研究所 1962
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/7175/files/KJ00002476097.pdf
https://doi.org/10.15094/00007175
https://nipr.repo.nii.ac.jp/records/7175
_version_ 1829308228349984768
author 福島, 博
フクシマ, ヒロシ
FUKUSHIMA, Hiroshi
author_facet 福島, 博
フクシマ, ヒロシ
FUKUSHIMA, Hiroshi
author_sort 福島, 博
collection National Institute of Polar Research Repository, Japan
description P(論文) The Kasumi Rock Ice-Free Area is located at 68°21'5"1.S. and 42°15'13"1.E. This area seems to have experienced not so many years since the glacial epoch, as no evidence of weathering nor weathered rocks were found there. Moss and lichen were not seen either. Only moraines were found in some places. 30 algae samples from 8 ponds were collected in polyethylene bottles. The time available for detailed investigation of the environmental factors was too short. The result is outlined in Table 1. The investigated ponds are 10-100 meters in diameter and less than 60cm in depth. The contents of nutritious salts (P, NH_3, N0_2) in these ponds are so small that a quantitative analysis was impossible, just like the case of the Shin-nan Rock Area. The SiO_2 content was 19-20 mg/l (standard). Ponds in the Kasumi Rock Area can be classified into two groups, one is of fresh water ponds and the other is of brackish water ponds. The former includes Stations 1 and 8, and the other has 5 stations (Stations 2-7). Concerning PH, the former was a little acidic and the latter was alkaline. The Kasumi Rock fresh water ponds contain much more Chlor ion than those of the Shin-nan Rock Area. Station 1 has 358 mg/l Chlor ion. In the brackish water ponds, the Chlor ion content varies with pond, and ranges from 4,959 to 9,523 mg/l. This is ca. 1/2-1/4 of Chlor ion in sea water. Almost all these brackish water ponds contain hydrogen sulfide and have a smell. Their bottom mud is black. In the ponds of the Kasumi Rock Area, blue-green algae and diatoms are predominant, whereas in the Shin-nan Rock Area only blue-green algae are found. The algal vegetation at Kasumi Rock is characterized by diatoms: Diatoms flora of the fresh water ponds differs from that of the brackish water ponds. The former belongs to the Navicula muticopsis association, and the latter to the Navicula cryptocephala var. intermedia-Navicula cryptocephala-Tropidoneis laevissima association. The writer found 46 taxon of diatoms in these ponds. Among 34 taxon already ...
genre Antarc*
Antarctica
Prince Olav Coast
genre_facet Antarc*
Antarctica
Prince Olav Coast
geographic Kasumi Rock
Prince Olav Coast
geographic_facet Kasumi Rock
Prince Olav Coast
id ftnipr:oai:nipr.repo.nii.ac.jp:00007175
institution Open Polar
language Japanese
long_lat ENVELOPE(42.250,42.250,-68.383,-68.383)
ENVELOPE(41.000,41.000,-69.000,-69.000)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00007175
op_relation 南極資料
15
1267
1280
AN00181831
00857289
https://nipr.repo.nii.ac.jp/record/7175/files/KJ00002476097.pdf
https://doi.org/10.15094/00007175
https://nipr.repo.nii.ac.jp/records/7175
publishDate 1962
publisher 国立極地研究所
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00007175 2025-04-13T14:07:44+00:00 ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ 南極大陸カスミ岩露岩地帯のケイ藻植生 NOTES ON DIATOM VEGETATION OF THE KASUMI ROCK ICE-FREE AREA, PRINCE OLAV COAST, ANTARCTICA 福島, 博 フクシマ, ヒロシ FUKUSHIMA, Hiroshi 1962-04 application/pdf https://nipr.repo.nii.ac.jp/record/7175/files/KJ00002476097.pdf https://doi.org/10.15094/00007175 https://nipr.repo.nii.ac.jp/records/7175 jpn jpn 国立極地研究所 南極資料 15 1267 1280 AN00181831 00857289 https://nipr.repo.nii.ac.jp/record/7175/files/KJ00002476097.pdf https://doi.org/10.15094/00007175 https://nipr.repo.nii.ac.jp/records/7175 1962 ftnipr https://doi.org/10.15094/00007175 2025-03-19T10:19:57Z P(論文) The Kasumi Rock Ice-Free Area is located at 68°21'5"1.S. and 42°15'13"1.E. This area seems to have experienced not so many years since the glacial epoch, as no evidence of weathering nor weathered rocks were found there. Moss and lichen were not seen either. Only moraines were found in some places. 30 algae samples from 8 ponds were collected in polyethylene bottles. The time available for detailed investigation of the environmental factors was too short. The result is outlined in Table 1. The investigated ponds are 10-100 meters in diameter and less than 60cm in depth. The contents of nutritious salts (P, NH_3, N0_2) in these ponds are so small that a quantitative analysis was impossible, just like the case of the Shin-nan Rock Area. The SiO_2 content was 19-20 mg/l (standard). Ponds in the Kasumi Rock Area can be classified into two groups, one is of fresh water ponds and the other is of brackish water ponds. The former includes Stations 1 and 8, and the other has 5 stations (Stations 2-7). Concerning PH, the former was a little acidic and the latter was alkaline. The Kasumi Rock fresh water ponds contain much more Chlor ion than those of the Shin-nan Rock Area. Station 1 has 358 mg/l Chlor ion. In the brackish water ponds, the Chlor ion content varies with pond, and ranges from 4,959 to 9,523 mg/l. This is ca. 1/2-1/4 of Chlor ion in sea water. Almost all these brackish water ponds contain hydrogen sulfide and have a smell. Their bottom mud is black. In the ponds of the Kasumi Rock Area, blue-green algae and diatoms are predominant, whereas in the Shin-nan Rock Area only blue-green algae are found. The algal vegetation at Kasumi Rock is characterized by diatoms: Diatoms flora of the fresh water ponds differs from that of the brackish water ponds. The former belongs to the Navicula muticopsis association, and the latter to the Navicula cryptocephala var. intermedia-Navicula cryptocephala-Tropidoneis laevissima association. The writer found 46 taxon of diatoms in these ponds. Among 34 taxon already ... Other/Unknown Material Antarc* Antarctica Prince Olav Coast National Institute of Polar Research Repository, Japan Kasumi Rock ENVELOPE(42.250,42.250,-68.383,-68.383) Prince Olav Coast ENVELOPE(41.000,41.000,-69.000,-69.000)
spellingShingle 福島, 博
フクシマ, ヒロシ
FUKUSHIMA, Hiroshi
ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ
title ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ
title_full ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ
title_fullStr ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ
title_full_unstemmed ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ
title_short ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ
title_sort ナンキョク タイリク カスミイワ ロガン チタイ ノ ケイソウ ショクセイ
url https://nipr.repo.nii.ac.jp/record/7175/files/KJ00002476097.pdf
https://doi.org/10.15094/00007175
https://nipr.repo.nii.ac.jp/records/7175