HIGH-SOLUTION STUDY ON LACUSTRINE SEDIMENTARY RECORDS FOR PAST 2000 YEARS IN CHINA:DEVELOPMENTS AND PROBLEMS
Received date: 1994-05-03
Online published: 1995-04-01
The regularities and causse of the earth environmental changes for past 2000 years are one of the major contents of the global change research. Compared with the other natural records, the lake sediments have the advantages of abundant information reserved, higher time solution and extensive geographic coverage. The studies on the Holocene lake sediments in respect to climatic and environmental changes have been carried on in China since 1980s, and are developing quickly now. As to the high-solution studies on lake sediments for past 2000 years, great attention should be paid to the several problems: (1)Improving the precision of nuclear dating technique;(2)Setting up the transfer function of the environmental proxies;(3)Understanding the early chemical diagenisis of the sediments;(4)Choosing stratified lakes and varved sediments;(5)Approaching the effective proxies for climatic elements;(6)Distinguishing the impact from human activities;and (7)Strenthing the spatial and temperal comparative studies.
Key words： Lacustrine sediments; Lake record; Past global change.
Ji Lei . HIGH-SOLUTION STUDY ON LACUSTRINE SEDIMENTARY RECORDS FOR PAST 2000 YEARS IN CHINA:DEVELOPMENTS AND PROBLEMS[J]. Advances in Earth Science, 1995 , 10(2) : 169 -175 . DOI: 10.11867/j.issn.1001-8166.1995.02.0169
[1] Eddy J A (ed). The PAGES Project:proposed implementation plans for reseach activities.IGBP Report No. 19,Stockholm ,1992. 112.
[2] 王苏民.湖泊沉积的信息、原理与研究趋势.见:张兰生(主编).中国生存环境历史演变规律研究.北京:海洋出版社，1993. 6-13.
[3] 周新宇，蔡述明，孔昭宸，杜乃秋.北京颐和园地区3000年来的植被与环境初探.见:张兰生(主编).中国生存环境历史演变规律研究.北京:海洋出版社.1993. 31-43.
[4] 王苏民，余源盛，吴端金，冯敏等.岱海——湖泊环城与气候变化.合肥:中国科学技术大学出版社，1990.
[5] 崔海亭，孔昭宸.内蒙古东中部地区全新世高温期气候变化的初步分析.见:施雅风(主编).中国全新世大暖期气候与环境.北京:海洋出版社，1993. 72-79.
[6] 孙湘君，袁绍敏.据花粉资料推断吉林金川地区最近1万年的植被演化.见刘东生(主编).黄土.第四纪地质•全球变化(第二集).北京:科学出版社，1990. 46-57.
[7] 刘金陵.长白山区孤山屯沼泽地13000年以来的植被和气候变化.古生物学报，1989,28(4):240-248.
[8] 吉磊，王苏民，郑长苏，羊向东，沈吉.浅钻岩心揭示的固城湖4000年来环境演化.湖泊科学，1993，5(3):316-323.
[9] 李文漪，刘光琇，周明明.湖北西部全新世温暖期植被与气候.见:施雅风(主编).中国全新世大暖期气候与环境.北京:海洋出版社，1993. 94-99.
[10] Jarvis D I. Pollen evidence of changing Holocene monsoon climate in Sichuan Province. China. Quat Res, 1993, 39,325-337.
[11] 王富葆，阎革，林本海.若尔盖高原泥炭δ13C的初步研究.科学通报，1993，38(1) : 65-67.
[12] 孙湘君，吴玉书.云南滇池地区全新世以来植被及环境变迁历史.见:中国—澳大利亚第四纪学术讨论会论文集. 北京:科学出版社，1987.
[13] Brenner M, Kathleen D, Song X, Wang Z, Long R, Binford M W, Whitmore T J, Moore A M. Paleolimology of Qilu Hu, Yunnan Province, China. Hydrobiology, 1991,214:333-340.
[14] Campo E V, Gasse F. Pollen-and diatom-inferred climatic and hydrological changes in Sumxi Co Basin (western Tibet)since 13000a B P. Quat Res,1993, 39:303-313.
[15] 顾兆炎，刘嘉麒，袁宝印，刘东生，刘荣谟等.1200。年来青藏高原季风变化——色林错沉积物地球化学的证据.科学通报，1993，38(1):61-64.
[16] 张彭熹，张保珍，杨文博.青海湖冰后期以来古气候波动模式的研究.第四纪研究，1989,(1):66-77.
[17] 王云飞.青海湖、岱海的湖泊碳酸盐化学沉积与气候环境变化.海洋与湖沼，1993,24(1):2431- 35.
[18] Lister G S, Kelts K, Chen K Z, Yu J Q, Niessen F. Lake Qinghai, China：closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene. Palaeogeogr Palaeoclimatol Palaeoeco1,1991,84：141-162.
[19] 杜乃秋，孔昭宸，山发寿.青海湖QH85-14C钻孔孢粉组合及其古气候古环境的初步探讨.植物学报，1989,31(10)：803-814.
[20] 周卫建，海德J.古土壤和湖相淤泥14C测年中有机质可靠性的讨论。见:刘东生(主编).黄土.第四纪地质.全球变化，第二集.北京:科学出版社，1990. 58-63.
[21] Aravena R，Warner B G. Carbon isotope composition of lake sediments in relation to lake productivity and radiocarbon dating. Quat Res,1992,37:333-345.
[22] Hillaire-Marcel C, Aucour A-M, Bonnefille R, Riollet G, Vincens A, Williamson D. 13C/palynological evindence of differential residence times of organic carbon prior to its sedimentation in East African rift lakes and peat bogs. Quat Sci Rev,1989,8:207-212.
[23] Krishnaswami S, Lal D.Radionuclide Limnochronology.In:Lerman A (ed.).Lakes chemistry, Geology, Physics. Now York: Heideberg. BerIin:Springer,1978.153-177.
[24] 项亮，王苏民.高纯锗井型探头r谱分析系统在甚年轻湖泊沉积年代学研究中的应用.见:中国第四纪南北对比与全球变化.第六届全国第四纪学术讨论会论文摘要汇编.广州:广东高等教育出版社，1993. 181-182.
[25] Webb III T,Bryson R A. Late-and post-glacial climate change in the Northern Midwest, USA:Quantitative estimates derived from fossil pollen spectra by multivariate stratistical analysis. Quat Res,1972,2:70-115.
[26] Bartlein P J,Webb III T,Fleri E. Holocene climatic change in the northern Midwest:pollen-derived estimates.Quat Res, 1984,22:361-374.
[27] Huntley B,Prentice I C. July temperatures in Europe from pollen data, 6000 year before present. Science,1988,241-687-690.
[28] Charles D F,Binford M W,Furlong E T, Hites R A, Mitchell M J. Paleoecological investigation of recent lake acidification in the Adirondack Mountains, N Y,1990.J Paleolimnol,1990,3:195-241.
[29] Fritz S C,Juggins S,Battarbee R W,Engstrom D R. Reconstruction of past changes in salinity and climate using a diatom-based transfer function.Nature,1991,352:706-708.
[30] Cohen A S,Dussinger R,Richardson J. Lacustrine paleochemical interpretations based on Eastern and Southern African ostracodes. Palaeogeogr Palaeoclimatol Palaeoecol,1983,43:129-152.
[31] 沈才明，唐领余.长白山、小兴安岭地区全新世气候—花粉—气候转换函数的初步研究.见:施雅风(主编).中国全新世大暖期气候与环境.北京:海洋出版社，1993. 33-39.
[32] Engstrom D R,Swain E B, Kingston J C. A palaeolimnological record of human disturbance from Harvey's Lake.Vermont: geochemistry,pigmerits and diatoms. Freshwat Bio1,1985,15:281-288.
[33] White J R,Gubala P. Sequentially extracted metal in Adirondack lake sediment core. J Paleolimnol,1990,3:243:252.
[34] Sanger J C. Fossil pigments in paleoecology and paleolimoology. Palaeogeogr Palaeoclamatol Palaeoecol,1988,62:343-359.
[35] Anderson R Y, Dean W E. Lacastrine varve formation through time. Palaeogr Palaeoclamatol Palaeoecol,1988,62:215-235.
[36] 陈振楼，黄荣贵，万国江.红枫湖沉积物—水界面Fe, Mn的分布和迁移特征.科学通报，1992,37(21):1974 -1977.
[37] De Deckker P,Forester R M. The use of ostracods toreconstruct continental palaeoen vironmental records. In:De Decker P, Colin J, Feypouquet 1 (ed.).Ostracoda in the Earth Sciences. Amsterdam:Elsevies,1988. 175-198.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
