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The Prince Gustav Channel was named in 1903 after Crown Prince Gustav of Sweden (later King Gustav V) by Otto Nordenskiöld of the Swedish Antarctic Expedition. The channel is bounded on the west by the Antarctic Peninsula and on the east by James Ross Island. It is about long and ranges from wide. On 27 February 1995, the British Antarctic Survey (BAS) reported that an ice shelf formerly blocking the channel had disintegrated. This ice shelf had spanned approximately prior to its disintegration.〔(Correll, Robert C. (1998). ''Our Changing Planet'', p. 90. DIANE Publishing. )〕 In the area previously covered by the shelf, the channel's water depth is between . Between February and March 2000, scientists collected sediment cores 5 to 6 m in length from the ocean floor. Carbon dating of organic material found in the sediment layers suggested that for a period between 2,000 to 5,000 years ago, much of the channel was seasonally open water. While icebergs were able to navigate the channel, ice rafted debris was deposited within the sediment. It appears that before and after this period, the channel remained closed. The period when the channel was open coincides with a period of local warming supported by data gathered from land-based studies of lake sediments and ancient, abandoned penguin rookeries. With the return of colder conditions about 1900 years ago, the Prince Gustav Ice Shelf reformed until its recent retreat and collapse. Ice shelves are sensitive indicators of regional climatic change, therefore recent warming in the vicinity of the Prince Gustav Channel is exceptional for at least the past 1900 years. ==References== 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Prince Gustav Channel」の詳細全文を読む スポンサード リンク
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