收稿日期: 1998-09-28
修回日期: 1999-03-09
网络出版日期: 1999-08-01
基金资助
本文得到中国科学院南京地理与湖泊研究所湖泊沉积开放实验室和中国博士后科学基金资助。
THE LAKE SEDIMENTS RESPONSES TO ENVIRONMENTAL AND CLIMATIC CHANGE
Received date: 1998-09-28
Revised date: 1999-03-09
Online published: 1999-08-01
李玉成,王苏民,黄耀生 . 气候环境变化的湖泊沉积学响应[J]. 地球科学进展, 1999 , 14(4) : 412 -416 . DOI: 10.11867/j.issn.1001-8166.1999.04.0412
The relative significance of the 20th-century climatic and environmental changes must be assessed from the long-term global-scale perspective available from a spectrum of proxy histories,including those from lake sediments. Lake sediments are sensitive to palaeoclimatic and palaeoenvironment change and record quantitative information about the processes and forcing factors responsible for producing both abrupt and long-term climate variation. Lake sediments also offer the best potential for a comprehensive interhemispheric comparision with a temporal resolution of decades-to-centuries .In many cases new geochemical proxies (biogenic carbonate, biogenic silica, organic matter indices) are needed to supplement the established use of stable isotope analyses for palaeotemperature and palaeohydrological modeling to understand the past environment conditions and evaluate predicative models of climate.
〔1〕Kelts K.湖沼沉积——过去变化的的信息库〔J〕.丁仲礼译.第四纪研究, 1992, (2):138～143.
〔2〕Fischer A G,de Boer P L, Premoli-silva I. Cyclostratigraphy〔A〕. In: Ginsburg R N,et aleds. Cretaceous Resources Events Rhythms〔C〕. NATO ASI Series C. Dordrecht:Kluwer Academic Publishers, 1989, No.304. 139～172.
〔3〕Emiliani C. Pleistocene temperature〔J〕. J Geol, 1955, 63(6): 539～578.
〔4〕Shackleton, N J, Opdyke N D. Oxygen isotope and paleomagnetic stratigraphy of Equatorical Pacific core V28-239,Late Pliocene to Latest Pleistocene〔A〕. In: Cline R M, Hays J O,eds. Investigation of Late Quaternary Palaeoceanography and Palaeoclimatology〔Z〕. Geological Society of the American Memoirs, 1976,145: 449～464.
〔5〕吴敬禄,王苏民.青藏高原RM孔碳酸盐氧同位素揭示的末次间冰期气候特征〔J〕.科学通报,1996,41(17): 1 601～1 604.
〔6〕王苏民,薛滨.中更新以来若尔盖盆地环境演化与黄土高原的比较研究〔J〕.中国科学(D辑),1996,26(4):323～328.
〔7〕李玉成,徐永昌,沈平.淡水软体动物化石碳氧同位素组成及其在恢复古气候环境中的应用〔J〕.沉积学报,1990,8(2):105～111.
〔8〕Williams D F,Peck J,Karabanov A A,et al.Lake Baikal record of continental climate response to orbital isolation during the past 5 million years〔J〕. Science,1997, 278:1 114～1117.
〔9〕Grootes P M, Stuiver M, White J C. Comparison of oxygen isotope records from GISP2 and GRIP Greenland ice cores〔J〕.Nature ,1993, 366: 552～554.
〔10〕GRIP members. Climate instability during the last interglacial period recorded in the GRIP ice core〔J〕. Nature,1993, 364: 203～207.
〔11〕Thouveny N, Tacques L B, Bonifay E. Climate variations in Europe over the past 140 ka deduced from rock magnetism〔J〕. Nature, 1994, 371: 503～506.
〔12〕Thompson L G, Yao T D, Davis,et al. Tropical climate instability: The last glacial cycle from a Qinghai-Tibetan ice core. Science, 1997, 276: 1 821～1 825.
〔13〕王苏民,余源盛,吴瑞金,等.岱海-湖泊环境与气候变化.合肥:中国科技大学出版社,1990.1～191.
〔14〕安芷生,吴锡浩,卢演俦,等.最近18 000年中国古环境变迁.自然科学进展—国家重点实验室通讯(试刊),1990,(2):167～173.
〔15〕于革.湖泊资料对6 ka BP气候模拟的评价〔J〕.南京大学学报(自然科学版)(江苏第二届博士后学术大会论文专辑),1997,33:286～288.
〔16〕秦蕴珊,赵松龄.全球变化与陆架沉积〔J〕.沉积学报,1992,10(3):40～46.
〔17〕Dansgaard W, White J W C, Johnson S T. The abrupt termination of the Younger Dryas climate events〔J〕. Ibid,1989, 339(6225): 532～533.
〔18〕Dansgaard W. Stable isotopes in precipitations〔J〕. Tellus,1964,16:436～468.
〔19〕莱尔曼主编.湖泊的化学地质学和物理学〔M〕.王苏民等译.北京:地质出版社,1989.1～370.
〔20〕Fritz P, Morgan A V, Eicher U,et al. Stable isotope, fossil coleoptera and pollen stratigraphy in Late Quternary sediments from Ontario and New York state〔J〕. Palaeogeogra Palaeoclimate Palaeoeco, 1987, 58: 182～202.
〔21〕李玉成,徐永昌,黄宝玉.淡水软体动物壳质氧同位素组成与气候环境〔J〕.沉积学报,11(3):57～63.
〔22〕Epstein S, Buchsbaum R, Lowenstams H A,et al. Revised carbonate-water isotope temperature scale〔J〕. Geol Soc Amer Bull, 1953, 64: 1 315～1 326.
〔23〕Krishnamurthy R V, Bhattacharya S K, Kusumgar S.Palaeoclimatic changes deduced from13C/12C and C/N ratios of Karewa lake sediments,India〔J〕. Nature, 1986,323:150～152.
〔24〕Mook W G. Palaeotemperatures and chlorinities from stable carbon and oxygen isotopes in shell carbonate〔J〕. Palaeogeogra Palaeoclimate Palaeoeco,1971,9:245～263.
〔25〕张彭熹,张保珍,杨文博.青海湖冰后期水体环境的演变〔J〕.沉积学报,1998,6(2):1～14.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
