{"created":"2023-05-15T16:34:43.280454+00:00","id":7435,"links":{},"metadata":{"_buckets":{"deposit":"f8866069-7512-4bc8-99d2-8fa004ee8866"},"_deposit":{"created_by":2,"id":"7435","owners":[2],"pid":{"revision_id":0,"type":"depid","value":"7435"},"status":"published"},"_oai":{"id":"oai:nagasaki-u.repo.nii.ac.jp:00007435","sets":["18:105:369:536"]},"author_link":["31231","31230","31233","31228","31232","31229"],"item_3_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Distribution of Lipid Compounds in Sediments from Imari Bay"}]},"item_3_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1992-02-29","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"42","bibliographicPageStart":"23","bibliographicVolumeNumber":"46","bibliographic_titles":[{"bibliographic_title":"長崎大学教育学部自然科学研究報告"},{"bibliographic_title":"Science bulletin of the Faculty of Education, Nagasaki University","bibliographic_titleLang":"en"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Imari Bay lies in the north-western part of Kyushu with the Takasima Is. at the bay-mouth and the Fukushima Is, in the cetral bay, copening north-westward into Genkainada open sea. The bottom sediments were divided into four groups, that is , calcareous muddy sand, calcareous mud, mud, muddy sand, by the contents of mud and calcium carbonate. Eight sediment samples have been analysed for aliphatic hydrocarbons (n-alkanes), aliphatic alcohols (n-alcohols), 4-methyl-sterols and 4-desmethyl-sterols in term of their area distribution, and in relation to the types of sediments. Distribution of n-alkanes having a high odd/even carbon number preference with a maximum at n-C29 or n-C31 show a predomkinant contribution of terrestrial higher plants. L/H values (L≦n-C20,H≧n-C21) of n-alkanes for the calcareous sediments from the strait and the bay-mouth area are relatively high (L/H=0.13 at St. 3, 5). Low L/H value for the muddy sand from the bay head (L/H=0.10 at st. 8) due to an influx of terrigenous higher plants which contain high concentrations of ≧n-C21from the Arita and Imari rivers. n-Alcohols ranging from n-C14 to n-C28 show even carbon number predominance and a maximum at n-C22 or n-C24. These ≧n-C22 alcohols were derived from the higher plants of terrestrial source. In the lower molecular weright range (