The uppermost Middle and Upper Albian succession at the Col de Palluel, Hautes-Alpes, France: An integrated study (ammonites, inoceramid bivalves, planktonic foraminifera, nannofossils, geochemistry, stable oxygen and carbon isotopes, cyclostratigraphy)     

A.S. GaleP. Bown  M. CaronJ. Crampton  S.J. CrowhurstW.J. Kennedy  M.R. PetrizzoD.S. Wray 《Cretaceous Research》2011,32(2):59-130

An integrated study of the ammonites, inoceramid bivalves, planktonic foraminifera, calcareous nannofossils, geochemistry, stable carbon isotopes, and cyclostratigraphy is provided for the upper Middle to upper Upper Albian sucession exposed in the Col de Palluel section east of Rosans in Hautes-Alpes, France. The Albian-Cenomanian boundary interval described by Gale et al. at Mont Risou is re-examined, a total thickness of 370 m of the Marnes Bleues Formation. Zonal schemes based on ammonites, inoceramid bivalves, planktonic foraminifera, and calcareous nannofossils are integrated with the stable carbon isotope curve and key lithostratigraphic markers to provide a sequence of more than 70 events in the uppermost Middle Albian to basal Cenomanian interval. Time series analysis of the Al₂O₃ content of the 500 m Albian sequence present in the Col de Palluel and Risou sections reveals the presence of the 20 kyr precession, 40 kyr tilt, 100 kyr short eccentricity, and 406 kyr long eccentricity cycles. Correlation using planktonic foraminiferan and nannofossil data provide a link between the Col de Palluel and Risou sections and the Italian sequence at Gubbio, and in the Piobbico core. This provides a basis for the extension of the orbital time scale of Grippo et al. to the sequence. It reveals a major break in the Col de Palluel succession at the top of the distinctive marker bed known as the Petite Vérole that may represent as much as 2 Ma. It also provides a basis for the estimation of the length of the Albian Stage at 4.12 Ma, 0.8 Ma for the early Albian, 2.84 Ma for the Middle Albian, and 3.68 Ma for the late Albian substages.  相似文献   

Diatom Response to Global Warming in Douhu Lake,Southeast China     

LI Jingjing  WANG Luo  CAO Qi  Patrick RIOUAL  LEI Guoliang  CAI Binggui  ZHANG Jiaoyang  ZOU Yafei  YAN Yao  WAN Xiaoqiao  XIAO Jule 《《地质学报》英文版》2021,95(2):638-647

A large number of lacustrine sedimentary records indicate that global warming is the main factor leading to significant changes in diatom communities in lakes of the northern hemisphere.However,due to the intensification of human activities since 1850,some scholars have emphasized that the increasing lake trophic level may be the main reason for the changes in diatom communities.The debate is ongoing.In order to avoid falling into the complex relationship between diatom changes and the seasonal cycle that characterizes lakes in mid and high latitudes,we chose a lake located at a low latitude,where the relationship between diatoms and temperature is not indirect but direct.The diatom record spans the past ca.100 years and reveals that the abundance of Aulacoseira granulata increased from 1900 until 1985, replacing the previously dominant Aulacoseira ambigua.These changes are in agreement with the increasing trend in global temperature.Since 1985,the percentages of the small-celled Discostella stelligera and the benthic diatom Navicula heimansioides have increased,while Aulacoseira granulata has decreased.This latest shift is caused by further global warming.We conclude that warming is the main factor leading to changing diatom communities in Douhu Lake.  相似文献   

北极新奥尔松地区土壤中生物硅含量及形态特征          下载免费PDF全文

刘森冉祥滨  臧家业王能飞 《极地研究》2015,27(3):237-245

硅循环与碳循环密切相关,生物硅作为硅的重要载体,在全球硅循环中占有十分重要的地位。目前,人们对陆地生态系统的硅循环做了大量研究,但对极地地区硅的研究却极为少见。利用中国第五次北极考察获得的土壤与植物样品,对北极新奥尔松地区中国黄河站站基表层土壤中生物硅的含量及土壤和植被中生物硅(主要为植硅体)的形态进行了初步研究。主要结论为:北极新奥尔松地区中国黄河站站基附近表层土壤中颗粒有机碳的含量为1.00—69.3 mg·g-1,平均值为13.7 mg·g-1;颗粒有机氮含量为0.11—9.84 mg·g-1,平均值为1.43 mg·g-1;可溶态硅含量为3.90—26.3μg·g-1,平均值为10.7μg·g-1;生物硅含量为5.60—9.97 mg·g-1,平均值为7.56 mg·g-1,且其含量与土壤颗粒态有机碳和颗粒有机氮呈正相关关系,表明三者具有相似来源。北极表层土壤生物硅比温带、热带地区生物硅含量要高。植物样品中植硅体形态以帽形、圆形、平滑棒形、齿形、刺棒形和哑铃形等形态为主,大小在10—100μm之间。土壤样品中的植硅体主要来源于植物,形态分别为平滑棒形、刺棒形、圆形、哑铃形、鞍形、尖形和帽形,另外硅藻也是北极土壤中生物硅的组成部分,其中裸露土壤中藻类(羽纹纲硅藻)占生物硅的多数(93.3%)。对比发现,有植被覆盖的土壤中,土壤有机碳、可溶出态硅、生物硅含量和植硅体形态丰富度往往比无植被覆盖或寡植被区土壤高,这表明尽管该地区植被稀少,但植物生长对该地区土壤硅循环存在显著影响,值得进一步关注。  相似文献   

Factors driving the seasonal distribution of planktonic and epiphytic ciliates in a eutrophicated Mediterranean Lagoon     

Amel Dhib  Mounir Ben Brahim  Boutheina Ziadi  Fourat Akrout  Souad Turki  Lotfi Aleya 《Marine pollution bulletin》2013

We studied the distribution of planktonic and epiphytic ciliates coupled with environmental factors and microalgae abundance at five stations in Ghar El Melh Lagoon (Tunisia). Planktonic ciliates were monitored for a year and epiphytic ciliates were sampled during summer 2011 in concordance with the proliferation of the seagrass Ruppia cirrhosa. Ciliate assemblage was largely dominated by Spirotrichea followed respectively by Tintinnida of and Strombidiida. No significant difference was found in the distribution of ciliate species among the stations. Redundancy analysis indicates that abiotic factors (temperature and nutriments) have a significant effect on the dynamics of certain ciliates. For epiphytic ciliates, 4 species were identified: Tintinnopsis campanula, Aspidisca sp., Strombidium acutum and Amphorides amphora. Based on PERMANOVA analyses, ciliates exhibit significant correlations among months and stations. According to ACP, epiphyte distribution follows roughly those of R. cirrhosa and pH. Significant correlations were found between harmful dinoflagellates and both planktonic and epiphytic ciliates.  相似文献   

Paleoceanographic changes of surface and deep water based on oxygen and carbon isotope records during the last 130 kyr identified in MD179 cores,off Joetsu,Japan Sea     

《Journal of Asian Earth Sciences》2014

We reconstructed the paleoenvironmental history of surface and deep water over the last 130 kyr from oxygen and carbon isotope ratios of planktonic and benthic foraminifera in two cores (MD179-3312 and MD179-3304) from the Joetsu Basin, eastern margin of the Japan Sea. Our data showed that paleoceanographic changes such as influx of surface currents and vertical circulation were associated with global glacial–interglacial sea level change. Surface water conditions were influenced by the influx of Tsushima Current, East China Sea coastal or off-shore waters through the Tsushima Strait during interglacial or interstadial stages, and strongly affected by freshwater input during the glacial maximum. During interglacial maximums such as Marine Isotope Stages 1 and 5e, development of well-oxygenated bottom water was indicated. A density-stratified ocean with weak ventilation was inferred from the isotopic records of benthic foraminifera during the Last Glacial Maximum. Local negative excursions in carbon isotopes during deglacial or interglacial periods may suggest the dissolution of gas hydrates or methane seep activities.  相似文献   

基于湖积物硅藻与地球化学记录的古环境变迁反演——以桂林会仙岩溶湿地为例     

汪良奇  张强  萧良坚  扈治安  李红春  谢运球 《中国岩溶》2014,33(2):129-136

通过对狮子潭柱状沉积物的放射性定年、地球化学与硅藻分析,反演桂林会仙岩溶湿地全新世的古湖沼演替,与其响应的气候变迁与人类活动记录。放射性210Pb、14C定年结果显示该湖在6 400 cal BP开始有湖积物保存,在2 700 cal BP—公元1943年间有沉积间断事件,且于公元1943年再度沉积。在6400—5 200 cal BP,高比例的浮游型硅藻反映高水位状态,可对应到气候暖湿的中国全新世大暖期鼎盛期。在5 200—2 700 cal BP,沉积物内稀酸可溶相Ca、Mg、Sr浓度降低,Mg/Ca、Sr/Ca值明显增加,且浮游型硅藻几乎消失,显示当时湖泊水位显著降低,气候逐渐变干。在公元1943年沉积物再度沉积,可能与战争造成人口迁徙与废耕有关。自公元1973年以来,硅藻壳片大量堆积,反映人类过度活动造成藻华的现象。湖泊沉积物内硅藻组成及沉积物的地球化学特征能够很好地反演古气候、环境变迁。  相似文献   

20万年来南海古海洋研究的主要进展     

李琪  李前裕  王汝建 《地球科学进展》2012,27(2):224-239

南海第四纪古海洋学的研究,从ODP184航次以来获得了快速的发展,已经成为国内外古海洋研究的重点地区之一。试图对国内外文献作一综述,介绍近20万年以来高分辨率的南海古海洋研究进展。综述主要涉及温度、盐度、生产力和上层水体的变化,重点介绍南海季风的研究成果。南海浮游有孔虫氧同位素曲线具有MIS3.3和MIS6.5期偏轻,MIS5.5和MIS7.3期偏重的特征,已被称为"季风型氧同位素曲线"。不同于代表全球冰量变化的底栖有孔虫氧同位素曲线(即SPEC-MAP曲线),"季风型氧同位素曲线"具明显的2万年岁差周期,代表了季风降水的影响。快速气候变化事件也有较为完整的记录,揭示了热带地区在快速气候变化中也发挥着重要的作用。  相似文献   

Phytoplankton abundance and community structure in the Antarctic polar frontal region during austral summer of 2009     

SHRAMIK Patil  RAHUL Mohan  SUHAS Shetye  SAHINA Gazi 《中国海洋湖沼学报》2013,31(1):21-30

The Antarctic polar front region in the Southern Ocean is known to be most productive. We studied the phytoplankton community structure in the Indian sector at this frontal location during late austral summer (February, 2009) onboard R/V Akademic Boris Petrov. We used the phytoplankton and microheterotrophs abundance, as also the associated physico-chemical parameters to explain the low phytoplankton abundance in the study region. This study emphasizes the shift of phytoplankton, from large (>10 μm) to small (<10 μm) size. The phytoplankton abundance appears to be controlled by physical parameters and by nutrient concentrations and also by the microheterotrophs (ciliates and dinoflagellates) which exert a strong grazing pressure. This probably reduces small (<10 μm) and large (>10 μm) phytoplankton abundance during the late austral summer. This study highlights the highly productive polar front nevertheless becomes a region of low phytoplankton abundance, due to community shifts towards pico-phytoplankton (<10 μm) during late austral summer.  相似文献   

黄海水母旺发区浮游鞭毛虫和纤毛虫群落结构分布及其与水母发生关系初探   总被引：2，自引：2，他引：0  

丁军军  徐奎栋 《海洋与湖沼》2012,43(3):527-538

鞭毛虫和纤毛虫在海洋微食物环和经典食物链间的能量流动中起着重要的枢纽作用,但其在水母暴发过程中的作用仍然不明。本研究基于2011年春季以及水母旺发的夏季黄海专项航次,通过荧光染色技术和定量蛋白银法研究了南黄海水母频发海域3个断面(E:33°N,G:34°N,I:35°N)的鞭毛虫和纤毛虫的群落结构和时空分布特点,对其与水母的发生关系进行了初步探讨。结果表明,春夏两季的微型鞭毛虫丰度均以近岸水域为最高,向外海递减,高值区大多出现在水体表层及底层附近。夏季总微型鞭毛虫的丰度和生物量较春季略高,且异养微型鞭毛虫比例升高。纤毛虫丰度的水平分布与鞭毛虫正相反,以近岸较低,向外海递增,主要分布在表层及10m水层。在水母出现的E和G断面,夏季纤毛虫数量显著降低,丰度仅为春季的30%—40%;而未见水母的I断面夏季较春季的数量升高了一个数量级。推测夏季水母发生的E、G断面纤毛虫丰度明显降低系因水母的捕食压力所致,纤毛虫数量的减少导致对鞭毛虫的摄食压力降低,鞭毛虫数量增加;而未见水母的I断面纤毛虫则维持较高的丰度值。本研究表明,水母作为浮游生态系统的顶级捕食者,可通过营养级联效应对微小型浮游动物群落产生影响。  相似文献   

白令海特征区域的表层沉积硅藻分布及其古海洋学意义   总被引：1，自引：1，他引：0  

黄元辉  石学法  吕华华  陈志华  程振波 《海洋学报》2012,34(3):106-113

对白令海表层沉积物样品进行硅藻分析,共鉴定硅藻30属56种(含变种),并确定17种硅藻新记录,其中包括Kisseieviella carina等3种化石种。白令海表层沉积物中的硅藻优势种为Neodenticula seminae,Fragilariopsis cylindrus和Fragilariopsis oceanica,在白令海北部陆坡深水区附近以Neodenticula seminae为主,而在白令海北部陆架以Fragilariopsis cylindrus和Fragilariopsis oceanica为主。对硅藻结果进行聚类分析,可以划分出3个硅藻组合,硅藻组合Ⅰ代表海冰种硅藻组合,组合Ⅱ代表受阿拉斯加流影响的大洋浮游硅藻组合,组合Ⅲ代表上述两个硅藻组合之间的过渡组合。Fossula arctica是17种硅藻新记录之一,首次记录于白令海表层沉积物中,其百分含量分布趋势与Fragilariopsis cylindrus和Fragilariopsis oceanica的相近,在白令海北部陆架为11.7%~17.1%,而在陆坡深水区附近明显减少,是继Fragilariopsis cylindrus和Fragilariopsis oceanica之后白令海又一海冰指示种,并有望成为一种有效的海冰变化替代物运用于晚第四纪以来白令海海冰进退历史研究。  相似文献