黄龙钙华210Pb计年与现代沉积的环境变化研究   总被引：4，自引：2，他引：2  

王华  覃嘉铭  安德军  杨琰  孙海龙  林玉山  杨勋林  应启和  张清明 《地球学报》2010,31(2):216-222

本文以黄龙钙华岩芯为主要研究对象, 利用210Pb定年技术在测定年轻碳酸盐样品短时间尺度上的优势建立了研究区近100年来高精度的年代标尺及环境记录; 通过碳氧稳定同位素的分析, 讨论了钙华稳定同位素记录与器测气候数据的相关性特征, 并与其他定年技术所获得的结果进行了相互验证。研究区钙华δ18O在1908~2004年时段内的变化范围为?12.13‰~?10.42‰, 平均值为?11.23‰, 变化幅度达到了1.7‰。同属西南季风区、由于海拔效应和距离水汽来源远近不同等因素的影响, 在同时段内黄龙钙华δ18O的变化范围和变化幅度都比董歌洞和Kahf Defore洞的δ18O记录要大, 说明处于中纬度、高海拔的黄龙钙华相对于低海拔的董歌洞和Kahf Defore洞石笋对气候环境的响应可能更加敏感。  相似文献   

闽浙沿岸海域春季溶解态稀土元素的分布和来源     

李换新  何会军  张劲 《中国海洋大学学报(自然科学版)》2021,(3)

通过2017年5月闽浙沿岸附近海域航次的温度、盐度和溶解态稀土元素(Rare Earth Elements,REEs)的实测数据,对该海域溶解态REEs的分布、配分模式以及主要影响原因进行了分析。结果表明:研究区域,盐度随着采样站位离岸距离的增加而增大。溶解态REEs则呈现近岸高而远岸低的分布特点。造成这种分布状况的原因:一是近岸陆源河流的输入导致近岸盐度低,REEs浓度高;二是受到高温高盐水(台湾暖流水和黑潮次表层水)的入侵,造成远岸盐度高而溶解态REEs元素浓度低。不同站位的溶解态REEs的配分模式有明显区别。近岸低盐站位由北向南,重稀土元素富集程度逐渐增大,反映了陆源不同河流的输入。通过溶解态REEs的配分模式发现,远岸高盐站位会受到台湾暖流和黑潮次表层水的共同影响。  相似文献   

Climatic variations in MIS 11 recorded by stable isotopes and trace elements in a French tufa (La Celle,Seine Valley)     

Julie Dabkowski  Nicole Limondin‐Lozouet  Pierre Antoine  Julian Andrews  Alina Marca‐Bell  Vincent Robert 《第四纪科学杂志》2012,27(8):790-799

Marine Isotope Stage (MIS) 11 palaeoclimate has so far been documented in marine and ice sheet isotopic records. However, excepting some lacustrine pollen records, very little is known about palaeoclimatic conditions in continental areas. This study uses geochemical records in calcareous tufa deposits from rivers as a basis for reconstructing temperate palaeoclimatic conditions. Tufa deposits are now proven to record high‐quality palaeoclimatic information in recent to Holocene deposits. Work on older interglacial tufas is just starting and in this paper we present the first comprehensive results from a MIS 11 tufa. The tufa comes from the Seine Valley (La Celle, northern France). Geochemical data in the tufa calcite are interpreted to record primarily air temperature (δ¹⁸O) and humidity (δ¹³C and Mg/Ca and Sr/Ca). The combined data identify a warm and wet climatic optimum followed by two temperature decreases associated with oscillations in humidity. These marked climatic variations recorded through the La Celle profile are strongly coherent with the palaeoenvironmental reconstructions from malacological data. The abrupt climatic and environmental events recorded could be related to short‐term degradation of vegetation cover in Europe, which is itself controlled by global palaeoclimatic events. Copyright © 2012 John Wiley & Sons, Ltd.  相似文献   

The evolution of the transboundary Evros river delta (Northeast Aegean Sea) under human intervention: a seven-decade analysis     

Aikaterini Karditsa  Athina Tsapanou  Serafim E. Poulos 《自然地理学》2020,41(4):291-314

ABSTRACT

The Evros deltaic plain (North Aegean Sea, Greece) covers an area of 188 km² and is shared by Greece and Turkey by its current main channel. This paper investigates deltaic plain evolution during the last seven decades (1945–2017), taking into consideration human interventions and their impacts on deltaic processes. Outcomes indicate that the construction of more than 25 major dams in the Evros River catchment resulted in >80% reduction in fluvial suspended load. Moreover, the alignment and relocation of the main distributary channel to the southeast was accompanied by the transformation of >40% of the deltaic plain to agricultural land. The combination of human interventions supports the coastline advance of the active main mouth (current rate of 3.9 *10^?3 km²/yr), retreat of the old (abandoned) Evros mouth (current rate 7.7 *10^?3 km²/yr), and signs of remarkable vulnerability in the middle mouth area.  相似文献   

Nitrogen budget in the Changjiang River drainage area     

江涛  俞志明  宋秀贤  曹西华 《中国海洋湖沼学报》2012,30(4):654-667

We established a budget model of nitrogen (N) inputs and outputs between watersheds and waterbodies to determine the sources of riverine N in the Changjiang (Yangtze) River drainage area. Nitrogen inputs in the budget included N from synthetic fertilizer, biological fixation by leguminous and other crops, wet/dry atmospheric deposition, excreta from humans and animals, and crop residues. The total N input was estimated to be 17.6 Tg, of which 20% or 3.5 Tg N was transported into waterbodies. Of the total N transported into waterbodies, the largest proportion was N from animal waste (26%), followed by N from atmospheric wet/dry deposition (25%), synthetic fertilizer N (17%), N in sewage wastes (17%), N in human waste from rural areas (6%) and industrial wastewater N (9%). We studied the spatial patterns of N inputs and outputs by dividing the Changjiang River drainage area into four sub-basins, from upstream to downstream: the Tongtian River drainage area (TTD, the headwater drainage area, 138 000 km 2 , less disturbed by human activities); the Jinsha River drainage area (JSD, 347 000 km 2 , less disturbed by human activities, approx. 3 500 km upstream of the Changjiang estuary); the Pingshan-Yichang drainage area (PYD, 520 500 km 2 , large-scale human disturbance, about 2 000 km upstream of the Changjiang estuary); and the Yichang-Datong drainage area (YDD, 699 900 km 2 , large-scale human disturbance, approx. 620 km upstream of the Changjiang estuary). The average N input into waterbodies was 2.3, 7.3, 24.1, and 28.2 kg N/ha in the TTD, JSD, PYD, and YDD sub-basins, respectively, suggesting an increase of N-components of more than 10 times from upstream to downstream areas.  相似文献   

A 12.8-ka-long palaeoenvironmental record revealed by subfossil ostracod data from lacustrine freshwater tufa in Lake Sinijärv,northern Estonia     

Kadri Sohar  Volli Kalm 《Journal of Paleolimnology》2008,40(3):809-821

High-resolution quantitative analysis of ostracod assemblages from 4.3-m-thick freshwater tufa-rich sediments, deposited during the last 12.8 ka in Lake Sinijärv, northern Estonia, yielded information on water level, trophic state conditions, and temperature changes since the late glacial. AMS ¹⁴C dates from aquatic mosses provided time constraints on the palaeoenvironmental development of the region. In the ostracod assemblage structure, four faunal zones (OFZ) were determined. The most significant change in the ostracod fauna occurred at 10,590 cal. y BP, when a typical littoral, polythermophilic fauna was replaced by a mostly sublittoral, species-rich meso- to stenothermophilic fauna. The ostracod data indicate two major low-water-level periods in the lake at 12,800–10,590 and 7,600–3,700 cal. y BP. Sediment analysis indicates the most intensive tufa precipitation occurred during these low stand periods, rather than during the warmest climate in Estonia between 8,000 and 4,500 cal. y BP. The late glacial low water level in the groundwater-fed Lake Sinijärv at 12,800–10,590 cal. y BP coincides partly with the regression in the Lake Peipsi basin (14,000–12,100 cal. y BP) and with the last drainage event of the Baltic Ice Lake at 11,600 cal. y BP. The low-water-level period in Lake Sinijärv occurred earlier than in lakes in the SE sector of Scandinavian glaciation. The change from low to high water level in Lake Sinijärv at 10,590 cal. y BP preceded the first post-glacial transgression events in the small lowland lakes of Estonia, southern Sweden, Poles`ye in Belarus, and Valday in NW Russia. In general, the mid-Holocene low-water-level period in Lake Sinijärv between 7,600 and 3,700 cal. y BP is concurrent with the regressions in the lakes of the SE sector of Scandinavian glaciation.  相似文献   

A note on radioactive riverine placers around Midtul,Bastar craton,Central India     

Yamuna Singh  K. Shiv Kumar 《Journal of the Geological Society of India》2009,73(3):419-424

Reconnaissance survey in the Midtul area (toposheet no. 65F/1; 18°52′30″N: 81°09′55″E) of the Bastar district, Chhattisgarh, revealed well-developed, 1 to 4 m thick riverine placers, derived from granitic terrain in the environs of the Mari River. The sediments comprise largely unconsolidated, cross-stratified gravels, sands, and silts, with low flat-topped surfaces which, at places, correspond to the morphology of terraces that are preserved on convex banks of the present day meanders, indicating their deposition by fluvial processes as channel bars. Available field data suggest deep-seated secular weathering of granites of the area, extensive reworking of such weathered products by fluvial processes, and their deposition as riverine placers in the vicinity of the streams draining the area. The granitic rocks of the area record radioactivity of 0.01–0.02 milli Roentgen per hour (mR/hr), with spots of higher radioactivity of 0.04–0.08 mR/hr, whereas riverine placers derived from them show radioactivity up to 0.25 mR/hr. Hand-panned polymineral concentrates from such placer deposits, analyzed by wavelength-dispersive x-ray fluorescence (WDXRF) spectrometry, showed 0.006–0.67 (n = 47; av. 0.092) % Y₂O₃ and 0.019–4.729 (n = 46; av. 0.834) % Ce₂O₃, with low values of Nb (41–467; n = 15; av. 197 ppm), Ta (115–598, n = 13; av. 230 ppm), and Sn (17–468; n = 14; av. 104 ppm). From the observed heavy mineral assemblage of monazite, zircon, ilmenite, epidote, hematite, and magnetite, as revealed by x-ray diffraction (XRD) studies, it is clear that the radioactivity is contributed by cerium, besides monazite (a phosphate of La, Ce, Th), and yttrium, possibly by zircon. Small amounts of niobium, tantalum, and tin are considered to be associated with ilmenite, epidote, and biotite. An occasional higher value of cerium (∼5% Ce₂O₃), together with restricted higher radioactivity, indicates only localized and uneconomic concentration of light REE-bearing mineral, monazite in isolated patches in such riverine placers.  相似文献   

Tufa as a record of perennial fresh water in a semi-arid rift basin, Kapthurin Formation, Kenya     

CARA ROURE JOHNSON  GAIL M. ASHLEY†  CAROL B. DE WET‡  RACHEL DVORETSKY‡  LISA PARK§  VICTORIA C. HOVER¶  R. Bernhart Owen  SALLY MCBREARTY 《Sedimentology》2009,56(4):1115-1137

Lithological and biological features of a fossiliferous tufa in the Kapthurin Formation, Baringo, Kenya, reveal the presence of a lush wetland in a semi-arid environment during the Middle Pleistocene ( ca 500 ka) in this portion of the East African Rift Valley. Four geological sections, each between 3 m and 8 m in thickness, exposed over a distance of 0·5 km, reveal a 1 to 2 m thick paludal tufa which is composed of three carbonate beds, two dark grey silty claystones and a reddish-brown silty palaeosol. High resolution stratigraphic analysis, carbonate petrography, stable isotope and elemental geochemistry, clay mineralogy and fossil remains (molluscs, ostracods, diatoms and charophytes) reveal a ground water-fed system that fluctuated in depth and periodically disappeared altogether. Oxygen isotope ratios (δ¹⁸O) of tufa matrix range from −4·5‰ to −8·0‰ (Vienna Pee Dee Belemnite) and become more positive up section, indicating the decreasing influence of fault-related fluids and increasing residence time or freshness of wetland water, rather than evaporative enrichment. This spring was situated on a lake margin during low lake levels, thrived during periods of increased ground water input and was ultimately replaced by an alkaline lake. The wetland would appear to have existed during a cool interval within the generally warm Marine Isotope Stage 13 or perhaps during the warm second half of Marine Isotope Stage 13. The ground water source of this wetland arose through a fault system. Thus, the position of the tufa deposit is controlled structurally but the timing and duration of the wetland system may have been influenced by both climatic and tectonic factors.  相似文献   

Sedimentology of coexisting travertine and tufa deposits in a mounded geothermal spring carbonate system,Obruktepe, Turkey   总被引：1，自引：0，他引：1       下载免费PDF全文

Benjamin Lopez  Gilbert Camoin  Mehmet Özkul  Rudy Swennen  Aurélien Virgone 《Sedimentology》2017,64(4):903-931

The recent discoveries of deeply buried Cretaceous reservoir bodies in the Atlantic Ocean revealed that relationships between the distribution of spring carbonate deposits and faults are poorly understood. The well‐exposed Quaternary deposits at Obruktepe (Denizli Basin, Turkey) provide an opportunity to reconstruct the three‐dimensional sedimentary architecture of such a system. Integration of sedimentological, lithofacies and geochemical analyses reveals complexity in the lateral relationships between sedimentary environments, faults and geothermal spring carbonates. Five environmental systems are distinguished based on the lithofacies analysis: (i) vent; (ii) smooth slope; (iii) travertine‐terrace; (iv) tufa‐barrage; and (v) flood systems. Encrusting, baffling and settling sedimentary processes are reflected in data acquired at several scales, from lithofacies observations to the morphology and arrangement of geobodies, together with microfabrics and stable carbon and oxygen isotope data. Mean values of +4·9‰ δ¹³C and −8·74‰ δ¹⁸O Vienna PeeDee Belemnite reflect geothermal circulation of springwaters. The environmental distribution and lithofacies indicate a lateral continuum between travertine and tufa deposits within this hot spring system. This finding supports two depositional models in which water flow variation is the main control on both CaCO₃ precipitation and the resulting formation of travertine and tufa. The proposed models address the factors responsible for the development of these complex mound‐shaped carbonate spring deposits, and how they are related to fluid circulation at depth and in association with faults.  相似文献   

长江口北支倒灌影响区盐度预测经验模型   总被引：1，自引：0，他引：1       下载免费PDF全文

孙昭华  严鑫  谢翠松  李奇 《水科学进展》2017,28(2):213-222

为预测不同径流过程影响下的盐水入侵强度,以长江口南支上段为研究对象,采用实测资料和理论分析相结合,建立了以大通流量和农历日期快速估算氯度值的经验模型。首先,以徐六泾实测潮位资料结合调和分析理论,在考虑11个主要分潮情况下证明日均潮差为半月周期函数,提出了用农历日期估算日均潮差的方法;其次,采用东风西沙实测氯度资料,选用不同函数形式,分析了以支汊盐水倒灌为主的情况下日均氯度对径流、潮差的量化响应关系;最后,提出了指数函数形式的氯度预测经验模型,模型计算值与实测值之间的决定系数在0.8以上。提出的经验模型可由大通流量快速估算特定位置的盐度,为相关的工程和规划研究提供了便捷途径。  相似文献