冲绳海槽西北侧表层沉积物中微型腹足类的分布及其研究意义     

冯伟民  黄宝玉 《海洋科学集刊》1997,(39):123-133

冲绳海槽西北侧大陆架向大陆坡转折处表层沉积物中微型腹足类动物群具有混合的生态特征,这与现代海洋沉积环境并不一致。腹足类动物群中除少数种类为陆坡深海分子,多数种类属内陆架区或近岸浅水分子。因此,动物群主要反映了晚更新世末次冰期低海平面的海洋环境,而少数深海种类的混入应与黑潮暖流在冲绳北端所形成的上升流有关。根据本区腹足类在其他海区的时空分布规律,本文认为在更新世末次冰期,黑潮暖流仍对本区有重要影响，并控制着腹足类的分布。本区腹足类这种混合的生态特征是晚更新世末次冰期以来各种海洋动力环境叠加影响的结果。  相似文献   

山西榆社-太谷盆地上新世中晚期的植被与环境   总被引：5，自引：0，他引：5  

李小强  鹿化煜  李承森  王宇飞 《海洋地质与第四纪地质》2002,22(1):103-108

山西中、东部的榆社、太谷盆地发育了良好的上新世河湖相地层，其丰富的植物、鱼类和哺乳类化石为我们提供了一个古植被和古环境研究的理想场所。根据榆社盆地磁笥年表以及化石组合特征，榆社、太谷盆地约为5．5MaBP以来的套沉积、榆社张村组与太谷小白组的沉积时代相当，大约形成于3．5－2．3MaBP。从大约4．4MaBP开始，较高含量的云杉、冷杉花粉显示研究区已有暗针叶林生长，从3．5MaBP开始，暗针叶林有了较大的发展，存在大面积的暗针叶林纯林。大致从上新世中期的4．4MaBP开始，气候已经开始变冷，并有较明显的干湿波动，蒿、藜为主的干草原大约从2．3MaBP开始繁盛，表明研究区转变为干冷气候。  相似文献   

日本海古海洋环境的演化     

余煦明 《海洋地质前沿》2005,21(8):6-9

基于近年来有关日本海的古海洋古环境研究成果，总结概述了日本海中新世以来的古气候和古海洋环境演化特征。日本海作为西北太平洋一个主要的边缘海，在全球气候变化过程中起着重要的作用。它的古气候古环境演化，与全球其他地区一样受控于地球轨道参数的变化，同时也发育一些由气候的不稳定性、海峡的开合与其他一些地球气候系统的非线性活动所驱动的突发性快速气候变化事件。日本海的古海平面、古海水温度、古洋流等因子的变化还受到冰盖扩张和退缩、构造运动、冰川性地壳均衡补偿、东亚季风等因素的影响，具有鲜明的区域特点。总体说来，目前对日本海的研究程度还不高，对它在全球气候变化中的作用过程、驱动和响应机制的了解还很有限，需要进一步深入研究。  相似文献   

Sedimentary facies and paleoenvironmental interpretation of a Holocene marsh in the Gironde Estuary in France     

WANG Jianhu  MASSE Laurent  TASTET Jean-Pierre 《海洋学报(英文版)》2006,25(6):52-62

1Introduction Since the last glacial maximum, the Holocenehas been marked by a rapid rise in sea level. After6 000 a BP, the present-day level was reached andthe rate of sea-level rise (SLR) decreased rapidly(Morzadec -Kerfourn, 1974; Kidson, 1986 ).These…  相似文献   

长江三角洲晚更新世末期古土壤与古环境   总被引：4，自引：0，他引：4  

刘宝柱  李从先  业治铮 《中国海洋大学学报(自然科学版)》1997,(3)

长江三角洲地区第一暗绿色硬粘土层是上海地区主要建筑持力层之一，也是划分全新统与更新统的标志层，前人已做过大量研究，但尚缺乏古土壤方面的系统研究工作。本文首次从古土壤学的角度系统研究了该层的古土壤特征，通过粒度分析发现有粘粒的生成，微形态研究发现有粘粒及铁锰、碳酸盐等化学组分的迁移与淀积，化学全量分析得出该层的硅铝率为２．８０～３．３７，说明该层已发生较强的成土作用，可以确认该层为古土壤层，并进一步把该层划分为４个Ｂ层、３个Ａ层，亦即该层为复合古土壤层。根据该层的成土特征，将其命名为古潮土  相似文献   

南海294站柱状沉积孢粉、藻类研究及古环境意义     

张玉兰  贾丽  孙煜华  郑玉龙 《海洋学研究》2003,21(1):5-12

通过对南海294站深海柱状剖面孢粉、藻类的研究,将294站从下至上划分为7个孢粉组合带: 带为Dacrydium-Pinus-Lithocarpus-Quercus(常绿)-Cyathea-Polypodiaceae; 带为Castanopsis-Lithocarpus-Dacrydium-Quercus(常绿)-Pinus-Polypodiaceae; 带为Quercus(常绿)-Castanopsis-Podocarpus-Cyathea-Polypodiaceae; 带为Polypodiaceae-Cyathea-Pteris-Pinus-Gramineae; 带为Quercus(常绿)-Podocarpus-Lithocarpus-Pinus-Cyathea-Polypodi-aceae; 带为Pinus-Quercus(常绿)-Palmae-Mangrovepollen-Gramineae; 带为Dacrydium-Palmae-Mangrovepollen-Pinus-Cyperaceae-Cyathea。相应恢复了南海东部地区12万年以来5个植被、气候演替阶段,依次为:炎热、湿润的热带季雨林—暖热而稍干的热带北缘半常绿季雨林—炎热、湿润的热带季雨林—暖热而稍干的热带北缘半常绿季雨林—炎热、湿润的热带季雨林。结合氧同位素测年资料,对南海294站柱状剖面地层时代划分进行了讨论。  相似文献   

THE　HOLOCENE　SEDIMENTAL　CHARACTERISTIC　AND　PALEOCLIMATIC　EVOLUTION　OF　EBINUR　LAKE，XINJIANG     

吴敬禄  王苏民  吴艳宏 《中国地理科学(英文版)》1996,(1)

ＴＨＥＨＯＬＯＣＥＮＥＳＥＤＩＭＥＮＴＡＬＣＨＡＲＡＣＴＥＲＩＳＴＩＣＡＮＤＰＡＬＥＯＣＬＩＭＡＴＩＣＥＶＯＬＵＴＩＯＮＯＦＥＢＩＮＵＲＬＡＫＥ，ＸＩＮＪＩＡＮＧ吴敬禄，王苏民，吴艳宏ＴＨＥＨＯＬＯＣＥＮＥＳＥＤＩＭＥＮＴＡＬＣＨＡＲＡＣＴＥＲＩＳＴ...  相似文献   

Environmental changes on Yugorski Peninsula, Kara Sea, Russia, during the last 12,800 radiocarbon years     

Andrei A. Andreev  William F. Manley   lafur Inglfsson  Steve L. Forman 《Global and Planetary Change》2001,31(1-4)

New pollen and radiocarbon data from an 8.6-m coastal section, Cape Shpindler (69°43′N; 62°48′E), Yugorski Peninsula, document the latest Pleistocene and Holocene environmental history of this low Arctic region. Twelve AMS ¹⁴C dates indicate that the deposits accumulated since about 13,000 until 2000 radiocarbon years BP. A thermokarst lake formed ca. 13,000–12,800 years BP, when scarce arctic tundra vegetation dominated the area. By 12,500 years BP, a shallow lake existed at the site, and Arctic tundra with Poaceae, Cyperaceae, Salix, Saxifraga, and Artemisia dominated nearby vegetation. Climate was colder than today. Betula nana became dominant during the Early Preboreal period about 9500 years BP, responding to a warm event, which was one of the warmest during the Holocene. Decline in B. nana and Salix after 9500 years BP reflects a brief event of Preboreal cooling. A subsequent increase in Betula and Alnus fruticosa pollen percentages reflects amelioration of environmental conditions at the end of Preboreal period (ca. 9300 years BP). A decline in arboreal taxa later, with a dramatic increase in herb taxa, reflects a short cold event at about 9200 years BP. The pollen data reflect a northward movement of tree birch, peaking at the middle Boreal period, around 8500 years BP. Open Betula forest existed on the Kara Sea coast of the Yugorski Peninsula during the Atlantic period (8000–4500 years BP), indicating that climate was significantly warmer than today. Deteriorating climate around the Atlantic–Subboreal boundary (ca. 4500 years BP) is recorded by a decline in Betula percentages. Sedimentation slowed at the site, and processes of denudation and/or soil formation started at the beginning of the Subatlantic period, when vegetation cover on Yugorski Peninsula shifted to near-modern assemblages.  相似文献   

Vertebrate Paleontology in Tibetan Plateau: Progress and Prospects     

WANG Xiaoming  LI Qiang 《《地质学报》英文版》2013,87(Z1):889-891

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Late Cenozoic paleovalley fill sequence from the Southern Liverpool Plains,New South Wales—implications for groundwater resource evaluation     

R. I. Acworth  W. A. Timms  B. F. J. Kelly  D. E. Mcgeeney  T. J. Ralph  Z. T. Larkin 《Australian Journal of Earth Sciences》2013,60(6):657-680

The Liverpool Plains in northern New South Wales contain some of the best agricultural land in Australia and are underlain by extensive smectite clay-dominated soils sourced from weathering the alkali basalts of the Liverpool Ranges. It had been thought that a relatively simple geological model explained the underlying Cenozoic sequence with salt-rich clays of the Narrabri Formation overlying sands and gravel aquifers comprising the Gunnedah Formation. Extensive groundwater modelling based upon this simple conceptualisation has been used in management plans proposed by the mining and agricultural industries. A 31.5 m core has been recovered using minimally disturbed triple-tube coring methods at Cattle Lane (Latitude –31.52° S, Longitude 150.47° E) to resolve uncertainty concerning the aquitard status of the upper layer. Recovered core has been examined and tested to determine grainsize, cation-exchange capacity, X-ray diffraction, X-ray fluorescence and microscopic examination of granular components. These measurements complement surface and borehole geophysical techniques, hydrogeological data and hydrochemical analysis of water samples recovered from a series of specially constructed piezometers adjacent to the cored hole. The sequence overlies a Late Cretaceous channel cut into Permian bedrock at 91 m depth with sands and clays below 31.5 m considered to represent various alluvial fill events mostly occurring since the Early Pliocene. Erosion of Late Eocene alkali basalts on the Liverpool Ranges, with the formation of smectite clays, pedogenic carbonates and with the addition of quartz from both eolian sources and locally derived from adjacent Triassic sandstone hills, provides the great majority of the sediment recovered from the cores. Late Pleistocene (114 ka) to Holocene ages were determined for the core from three optically stimulated luminescence (OSL) measurements on fine sands (13, 23 and 29 m BG). Detailed examination has failed to detect any evidence of a boundary between Narrabri and Gunnedah formations revealing rather a gradual change in dominance of clays and silts over sands and gravels embedded in a clay-rich matrix. This result challenges the conceptualisation used to conduct groundwater modelling on the Liverpool Plains.  相似文献