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苏北沿海平原第四纪沉积的孢粉组合与古植被、古气候 总被引：4，自引：0，他引：4
苏北沿海平原地势平坦广阔,河湖众多,其南界为长江北岸,南部江阴、南通有孤岛状低丘分布。本区气候温和,四季分明,年均温在13.5℃—15.5℃之间,年降水量为900—1,200毫米,是亚热带冬季低温而降水稍高的一个植被区。本区由于人类长期经济活动,农业栽培比较发达,自然植被很稀疏。原生植被除沿海的盐生植被外,极少保存。沿海盐土上主要植物有盐蒿(Suaeda salsa)、碱蓬(S.glauca)、羊角草(Salicornia herbacea)、大穗结缕草(Zoysia macrotachys)、獐茅(Aeluropus littoralisvar.sinensis)等。湖泊地区水生植被繁茂,主要有茨藻、眼子菜、狐尾藻、菱、金鱼藻、水 相似文献
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The palynolpgical study on the Quaternary sediments of 42 cores in the region of the Yangtze River Delta and the sections of 4 relics had been done since 1960. Palynological assemblages from the region of the Yangtze River Delta, showing obviously .common characteristics but with slight differences because of the vast areas covered, can be divided into five spores and pollen zones and three subzones in ascendant order:I.Quercus alienc-Pinus-Cupressaceae-Chenopodiaceae spores and pollen zone reflecting the cool, then cold and dry climate--Preboreal.II.Quercus dentata-Quefcus acutissima-Pinus-Castanea-Artemisia spores and pollen zone reflecting the temperate and cool, but a little dry climate--Boreal.III.Quercus glauca-Caslanopsis-Myrica-Caslanea spores and pollen zone reflecting the hot and moist climate--Atlantic.IV.Quercus acutissima-Pinus-Castanea-Quercus glauca- Chenopodiaceae spores and pollen zone reflecting the warm, and a little dry climate--Subboreal.V.Quercus acutissima-Costarica-Quercus glauca 相似文献
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长江三角洲全新世孢粉组合及其地质意义 总被引：13，自引：1，他引：13
长江三角洲是在河、海交错影响下的沉积,是世界上最大的三角洲之一.长江三角洲地区又是我国东部主要的工农业基地.因此,长江三角洲全新世沉积的研究对于含水层划分、工程地质评价、天然气等矿产调查及三角洲岩系研究(古三角洲沉积往往是油气聚集的有利地带)皆有一定意义.长江三角洲全新世地层其岩性主要为灰色、灰褐色和黄色粉细砂和亚粘土,下部相对较粗,以粉细砂及粘土粉细砂为主.其厚度各地不一,一般是由西南向东北变厚,常州、无锡、崑山一带约5—20米,而上海、崇明为20—50米,苏北长江沿岸最厚达40—60米. 相似文献
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PALYNOLOGICAL ASSEMBLAGES FROM THE QUATERNARY SEDIMENTS OF THE CHANGJIANG RIVER DELTA AND THE AGE OF STRATA AND PALEOGEOGRAPHY 总被引：2，自引：0，他引：2
Through the palynological research of Quaternary sediments in Changjiang River Delta, 14 spores and - pollen zones might be distinguished, reflecting the vegetation succession and climate fluctuation of Quaternary, which conforms to the climate of the world.Zones 1-9 are thought of as Pleistocene and Zones 10-14 as Holocene based on the climatic fluctuation reflected by these zones and the comparison with the climatic stage at home and abroad.The marine facies sediments of Quaternary in the Changjiang River Delta contain abundant fossil spores and pollen and have obvious characters. Because the warm and humid climate reflected by the palynological assemblages of marine facies sediments often fittes with the transgression, the curve line of the climate fluctuation of Quaternary in the Delta coincides with that of sea level changes. 相似文献
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