| 南极乔治王岛菲尔德斯半岛西湖柱状剖面藻类化石与环境演变 |
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| 引用本文： | 刘清泗,降廷梅.南极乔治王岛菲尔德斯半岛西湖柱状剖面藻类化石与环境演变[J].极地研究,1990,2(2):28-35. |
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| 作者姓名： | 刘清泗 降廷梅 |
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| 作者单位： | 北京师范大学地理系，北京师范大学地理系 北京 100875，北京 100875 |
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| 基金项目： | 国家南极考察委员会支持项目，并得到国家自然科学基金资助 |
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| 摘 要： | 根据西湖柱状岩芯样品中藻类化石的分布与含量变化,推测本区在3600年前仍为冰川覆盖;距今3600～3000年前为冰缘浅湖期;3000～1200年前湖水稳定,气候环境相对较好;距今1200年至现代气候略有波动。
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| 关 键 词： | 乔治王岛 藻类化石 环境演变 |
ALGAE FOSSILS IN SEDIMENTS OF WEST LAKE ON FILDES PENINSULA OF KING GEORGE ISLAND, ANTARCTICA, AND THE ENVIRONMENTAL EVOLUTION |
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| Liu Qingsi Jiang Tingmei.ALGAE FOSSILS IN SEDIMENTS OF WEST LAKE ON FILDES PENINSULA OF KING GEORGE ISLAND, ANTARCTICA, AND THE ENVIRONMENTAL EVOLUTION[J].Chinese Journal of Polar Research,1990,2(2):28-35. |
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| Authors: | Liu Qingsi Jiang Tingmei |
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| Abstract: | A large amount of Pediastrum and Bacillariophyta fossils were found in sediments of West Lake on Fieldes Peninsula of King George Island. Pediastrum fossils include the following species: Pediastrum Mey., P. boryanum (Turp.), P. simplex (Mey.) Lemm., P. duplex Mey., and Bacillariophta fossils include Melosira Ag., M. roeseana Rabh., M. roeseana var., Achnanthes Bory., A. lanceolata Breb., A. lanceolate, var. rostrata Hust., A. exigua var. heteroval-vata Krasske, A. delicatla (Ktz.) Grun., Navicula. Bory., N,dicephala (Ehr.) W.S., N. pseudos-cutiformis Hust., N., cuspidata Kutz., N. cryptocephala Kutz., N. anglica Ralfs, N. rhynchocephala Kutz., Stauroneis Ehr., S. anceps Ehr., S. anceps f. linearis (Ehr.) CI., Pinnularia Ehr., P. gibba var. subundulata Mayer, P. borealis Ehr., P. gibba var. linearis Hust., P. brevicostata CI., P. intermpta W. Smith, P. undulata Greg., P. microslauron (Ehr.) CI., Gomphonema Ag., G. angustatum (Kutz.) G. angustatum var. obtusatum V.H., G. parvulum var. micropus (Ktz.) Cleve., G. parvulum var. subelliptica CI., G. abbreviatum Ag., Hantzschia Grun., Surirelia Turp., Mtzschia frustulum (Ktz.) Grum., N. linearis W. Smith, Hantzschia amphioxys var. maior Grum., Synedra rumpens Ktz., pephora marty He'rib. and etc.
The distribution and content variation of the fossils along the sedimentary profile permit us to reach the following conclusions: about 3600 a. B.P., this area was covered with glaciers,because no algae fossils were discovered in this part of section at about 264-289cm depth; From 3600 to 3000 a B.P. it was dominated by a shallow periglacial lake, a few Pediastrum fossils were found in this part of section (a depth from 289 cm to 224 cm); And from 3000 to 1200 a B.P., the lake became deeper gradually and the climatic conditions were better, because a large amount of Pediastrum and Bacillariophyta fossils were found in this part of section (from 224 ot 87 cm) and these Algaes lived in fresh water; And from 1200 a B.P. to the present (from 87 cm depth of the section to the surface layer of the lake) the content of the fossils some varies. It shows that the lake level has fluctuated slightly. |
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| Keywords: | King George Island algue fossils environmental evolution |
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