共查询到20条相似文献，搜索用时 31 毫秒
1.
Santanu Banerjee Shovan Lal ChattorajP.K. Saraswati Somnath DasguptaUrbashi Sarkar 《Marine and Petroleum Geology》2012,30(1):144-160
Formation and maturation of glauconites within the early Middle Eocene Harudi Formation, built up in a lagoon to shelf transition in western Kutch, India is addressed taking recourse to a combined sedimentological, micropalaeontological and mineralogical investigation. The glauconite is authigenic and its occurrence coincides with maximum flooding. The glauconite is more matured within the fecal pellets and is less matured within the intra-particle pores of bioclasts namely, foraminifera, ostracoda, gastropoda and bryozoa. SEM-EDS, XRD and geochemical studies clearly document that the infilling within the intra-particle pores of bioclasts belong to nascent to slightly evolved glauconite (<5 wt% K2O), while the pellet belongs to slightly evolved to evolved glauconite (5-7 wt% K2O). Based on chemical characteristics and SEM investigations the glauconitization process can be best explained by the ‘verdissement theory’. The glauconite possibly formed as initial authigenic glauconitic smectite precipitates; while the pellet matured subsequently by addition of K, the process was hindered in case of infillings. The maturation process also involved addition of Si and release of Al, with or without release of Mg. The glauconite maturation was facilitated in case of fecal pellets because of higher porosity, inter-granular nature of pores and availability of necessary elements in semi-confined micro-environments. In contrast, the maturation was aborted at an early stage in case of infillings because of the minute, closed nature of the pores and prevalent alkaline conditions not allowing dissolution of calcitic tests. A low negative cerium anomaly suggests glauconite formation in sub-oxic micro-environments, created by decay of organic matters within the fecal pellets and bioclasts. A clear case of substratum control on glauconitization becomes apparent. 相似文献
2.
Generation, morphology, and distribution of authigenic minerals directly reflect sedimentary environment and material sources. Surface sediments were collected from the western Gulf of Thailand during 2011–2012, and 159 samples were analyzed to determine detrital minerals. Authigenic minerals, including siderite, pyrite, and glauconite, are abundant whereas secondary minerals, such as chlorite and limonite, are distributed widely in the study area. Siderite has a maximum content of 19.98 g/kg and appears in three types from nearshore to continental shelf, showing the process of forming-maturity-oxidation. In this process, the Mn O content in siderite decreases, but Fe_2O_3 and Mg O content increase. Colorless or transparent siderite pellets are fresh grains generated within a short time and widely distributed throughout the region; high content appears in coastal area where river inputs are discharged. Translucent cemented double pellets appearing light yellow to red are mature grains; high content is observed in the central shelf. Red-brown opaque granular pellets are oxidized grains,which are concentrated in the eastern gulf. Pyrite is mostly distributed in the central continental shelf with an approximately north–south strip. Pyrite are mainly observed in foraminifera shell and distributed in clayey silt sediments, which is similar to that in the Yangtze River mouth and the Yellow Sea. The pyrite in the gulf is deduced from genetic types associated with sulfate reduction and organic matter decomposition. Majority of glauconite are granular with few laminar. Glauconite is concentrated in the northern and southern parts within the boundary of 9.5° to 10.5°N and is affected by river input diffusion. The distribution of glauconite is closely correlated with that of chlorite and plagioclase, indicating that glauconite is possibly derived from altered products of chlorite and plagioclase. The K_2O content of glauconite is low or absent, indicating its short formation time. 相似文献
3.
An integrated study involving sedimentology, mineral chemistry and spectroscopy highlights a distinctive compositional evolution of Cretaceous glauconite within the Ukra Hill Member. Glauconite occurs at the top part of transgressive systems tract deposits built on a marine shelf. The concentration of glauconite steadily increases towards the maximum flooding surface, maximizing around 50%, and sharply falls at the onset of progradation. Unlike most Phanerozoic examples, Ukra glauconite forms by the variable degree of replacement of quartz, feldspar and mica grains. XRD, FEG-SEM and spectroscopy of glauconite pellets indicate an ‘evolved’ stage of maturation. Mossbauer spectroscopy reflects a minor substitution of Al3+-Fe3+ (total) in tetrahedral sites and significant substitution of the same in octahedral sites. A consistently high value of K2O as well as Fe2O3 contradicts the two popular theories, ‘layer lattice’ and ‘verdissement’, and support replacement origin of glauconite in a high aSi+ and high aK+ pore water environment. Incipiently formed glauconite records a marginal increase in K2O content accompanied by release of Al2O3 and SiO2 to form evolved glauconite pellets; those forming within quartz grains involve an addition of Fe2O3 (total) content during maturation. The minimal increase in K2O content of incipiently formed glauconite, best exhibited by those formed within quartz grains is possibly related to stratigraphic condensation. Compositional evolution like this is exhibited by Precambrian glauconites involving abiotic substrates, but is unusual for the Phanerozoic. Original K2O and Fe2O3 (total) content of glauconites is reduced around peripheries and fractures during diagenesis, adding to compositional variability. 相似文献
4.
David J. Cullen 《新西兰海洋与淡水研究杂志》2013,47(4):399-406
Radiometric analysis indicates that a granular variety of glauconite, widespread on the Chatham Rise, is derived from late Tertiary sediments. Other forms of glauconite, associated with pumice, phosphorite nodules, and glacially‐transported erratic blocks, are of Quaternary age. These are quantitatively unimportant, and may have originated as a result of redistribution of components from the older glauconite. 相似文献
5.
以马氏珠母贝(Pinctada fucata martensii)黄壳色作为选育指标构建了黄壳家系,对其4个生长性状和黄壳色性状分离比进行了统计分析,并测定了黄壳家系中黄壳、褐壳色个体不同组织中的总抗氧化能力(TAC)。结果发现:黄壳色性状能遗传并发生分离,其分离不完全符合孟德尔遗传分离定律;褐壳色亲本不会产生黄壳色子代,推测褐壳色是纯合子;第一代黄壳家系5、7月龄贝仅壳宽值显著小于褐壳家系(P0.05),壳高、壳长、总质量差异不显著, 11月龄贝仅壳长和壳宽值显著小于褐壳家系, 14、20月龄贝的壳高、壳长、壳宽、总质量这4个生长性状均极显著小于褐壳家系(P0.01);在第一代6个黄壳家系内,黄壳、褐壳色个体的4个生长性状差异不显著;黄壳色贝在足、心、性腺中的TAC显著低于褐壳色贝(P0.05);在鳃、闭壳肌、消化腺组织中TAC高于褐壳色贝,但差异不显著。 相似文献
6.
Fecal pellets are ubiquitous in sediment collected from deep ocean ridge, continental shelf and fjord-type estuarine environments
off the Canadian West Coast. Fecal pellets of the immature diagenetic stage are composed generally of the same mineral suite
as the bulk sea-bottom sample; except that degraded biotite and/or illite has absorbed Fe and K to regrade into glauconite.
These fecal pellets (<10 years old) contain 10 to 15% glauconite. Highly evolved monomineralic fecal pellets (e.g. glauconite,
smectite) of such modern age show that diagenetic minerals commonly associated with burial can be produced by sediment-organism
interactions. 相似文献
7.
The rough pen shell Pinna rudis Linnaeus, 1758 (family Pinnidae), a mollusc with an Atlantic–Mediterranean distribution, is able to live in coarse sandy substrates. Considering its shell structure and ecological characteristics, P. rudis can enhance biodiversity by providing a substrate for settlement on its shell. For this reason, we compared the diversity of benthic taxa around P. rudis shells with the species diversity on P. rudis shells, at Matiota Beach, São Vicente Island, Cabo Verde. We sampled an area of 900 m2 and recorded data in situ to estimate the population size of P. rudis and the epibiotic and benthic community diversity. The average density of P. rudis estimated in the sampled area was 6.6 ind. 100 m–2 and the highest density was found at between 2 and 3 m depth, mostly in biogenic and sandy substrates. The epibiotic species diversity on P. rudis shells was significantly higher than the species diversity in the microhabitat around the shells. The P. rudis shell seems to play an important role in increasing the biodiversity of the ecosystem, with some species found only as epibionts on P. rudis. 相似文献
8.
台湾海峡沉积物中海绿石的矿物学与分布特征 总被引：3，自引：0，他引：3
本文研究台湾海峡表层沉积物中海绿石的矿物学特征，分布格局及富集的沉积环境。结果表明，海峡海绿石系高硅富铁的含水硅盐矿的，为二八在体向三八面体过渡型结构类型，具有现代海绿石性质。海峡东北部，中部主要分布黑色颗粒海绿石，南部为灰绿色生物状海绿石。 相似文献
9.
The rich glauconite deposits off the south and west coasts of southern Africa originated by erosion of Cretaceous and Tertiary bedrock during mainly Tertiary transgressive/regressive cycles. This work, the first major electron microprobe investigation of glauconite, was undertaken to provide reliable chemical data of uncontaminated, unaltered glauconite pellets and to trace the chemistry of the glauconitization process.The data suggest that Fe is emplaced into the clay structure very early in the glauconitization process, possibly by a mechanism which is independent of and prior to the fixation of K. The sympathetic relationship between K2O and MgO indicates that some Mg is located in the interlayer position. 相似文献
10.
为研究硬壳蛤形态性状对体质量(Y)、软体质量(Y1)及肥满度(K)的影响,测量硬壳蛤的壳长(X1)、壳宽(X2)、壳高(X3)、体质量(Y)和软体质量(Y1)等指标,并进行相关性分析、多元回归分析和通径分析。结果表明:体质量变异系数最高,壳宽与体质量相关系数最高(0.970)、壳长与软体质量相关系数最高(0.946)、壳长与肥满度相关系数最高(0.203)。壳宽对体质量直接作用最大(0.145)、壳长对软体质量直接作用最大(1.113)、壳长对肥满度直接作用最大(1.752)。形态性状与体质量、软体质量及肥满度的多元回归方程分别为Y=–46.359+0.288X1+1.723X2+0.640X3,R2=0.949;Y1=–6.607+0.301X1+0.157X2–0.161X3,R2=0.901;K=3.159+0.173X1+0.008X2–0.179X3,R2=0.072。壳宽是影响硬壳蛤体质量的主要因素,壳长是影响硬壳蛤软体质量的主要因素,各性状与肥满度回归关系不显著,个体间肥满度差异大。研究结果可为硬壳蛤选育及苗种繁育提供参考。 相似文献
11.
I. D. Marsden 《新西兰海洋与淡水研究杂志》2013,47(2):359-370
Paphies donacina (Spengler, 1793) populations were surveyed at 11 low tide sites on surf beaches along Pegasus Bay, Canterbury, New Zealand, during summer 1998. Random sampling was not feasible. At the non‐random sites chosen the average number of tuatua per 5 m of shoreline ranged between 0.1 and 62. Total wet weight biomass m‐2 was highest at the southern sites in the Bay. There were site‐related differences in length frequency distributions of tuatua populations. Northern populations included a wide length range and southern populations were dominated by larger bivalves. Average shell length increased significantly with distance south, being close to 40 mm at Waikuku and 80 mm at Taylors Mistake. The shell length: width and weight relationships were similar for tuatua collected over the whole geographic range. Average dry weight condition index varied significantly between sites (ANOVA F= 23.3, d.f. = 10, 329) depending on the length distribution of the contributing population. Where populations included a wide length range the condition index was positively correlated with shell length but in populations dominated by larger bivalves there was either no relationship or a negative relationship with shell length. Juvenile tuatua were found at average densities between 81 and 1200 m‐2 at all sites except Taylors Mistake. The mean length of recruits ranged from 2.2 to 3.1 mm and shell length was independent of both juvenile and adult density. These results are discussed in relation to the environmental and other factors thought to influence population structure and recruitment of tuatua in Pegasus Bay. 相似文献
12.
采用相关分析、共线性分析、多元回归分析及通径分析的方法对日本镜蛤(Dosinia japonica)的壳尺寸性状与重量性状间的关系进行了研究。相关分析结果表明,所测量的日本镜蛤的各性状间均呈极显著的表型相关(P<0.01);共线性分析剔除了与各壳性状存在严重共线性的壳长;通径分析表明,壳高和壳宽是直接影响体重和壳重的主要性状,壳宽和b(壳顶至壳后)是直接影响软体部重和软体部干重的主要性状,而直接影响体积的壳尺寸性状只有壳高;采用逐步回归的方法,建立了壳尺寸性状对体积和重量性状的最优回归方程,可为日本镜蛤的养殖和选择育种提供理论依据。 相似文献
13.
紫扇贝和海湾扇贝杂交家系的生长和通径分析 总被引：2，自引：0，他引：2
以紫扇贝(Argopecten purpuratus)和海湾扇贝(Argopecten irradians irradians)为亲本,建立了紫扇贝自交(ZZ)、海湾扇贝自交(HH)、紫扇贝(卵)×海湾扇贝(精)(ZH)和海湾扇贝(卵)×紫扇贝(精)(HZ)共4个试验家系.在养殖60、127 d时测定壳高、壳长、壳厚和体质量,并分析各养殖时期影响体质量的主要因素.结果表明:在各养殖时期,2杂交家系子代的壳高、壳厚以及体质量均表现出生长优势(P＜0.01),因此认为通过紫扇贝和海湾扇贝杂交方式是改善扇贝的良好方法.通径分析的结果表明,对于自交家系,壳长是影响体质量的主要影响因素,但对于杂交家系HZ来说,壳长(60 d)和壳厚(127 d)对体质量的决定作用最大;在杂交家系ZH,60 d时壳长和壳厚的协同作用对体质量的决定作用最大,127d时壳高的决定作用最大.因此对于两个杂交家系的选育,应按照不同性状对体质量的决定系数选择各时期的优势性状,以使子代的杂种优势充分表现. 相似文献
14.
养殖条件下不同年龄背瘤丽蚌(Lamprotula leai)数量性状的相关与通径分析 总被引：1，自引：0，他引：1
随机选取养殖2龄、3龄和4龄的背瘤丽蚌(Lamprotula leai)各30个,分别测定壳长、壳高、壳宽、壳厚、活体重和壳重等数量性状参数并计算了各性状间的相关系数。应用Duncan法多重比较分析了不同年龄个体的形态差异,以壳重为因变量,其它数量性状为自变量进行多元回归和通径分析,计算了对应的通径系数和决定系数,并建立了最优回归方程。结果表明:2龄蚌和3龄、4龄蚌之间在形态上具有显著差异;不同年龄背瘤丽蚌各数量性状(2龄蚌壳厚除外)与壳重均极显著相关(P0.01);通过对各年龄段各种性状对壳重的通径分析和决定系数分析,发现活体重对壳重的通径系数分别为0.900、0.902和0.923,决定系数分别达到0.81000、0.81360和0.85193,是影响壳重最主要的性状。采用逐步回归法,剔除偏回归系数不显著的性状,建立了数量性状对壳重的最优回归方程。基于对壳重决定效应的大小,活体重可作为背瘤丽蚌良种选育的目标性状。 相似文献
15.
16.
K. B. Lewis 《新西兰海洋与淡水研究杂志》2013,47(3):183-208
Sediments from the seabed off the eastern side of the North Island, New Zealand, are divided into 12 facies on the basis of grain size and mineralogy of the sand fraction. The facies are grouped into three types; modern detrital sediments, relict detrital sediments, and non‐detrital sediments. The sediments are described in terms of a modified Wentworth grain‐size scale and a modified Folk sediment classification. The modern detrital sediments range from fine sand near the shore to clayey fine silt on the lower slope. At most places they are bimodal, probably because floes and single grains are deposited together. The relict detrital sediments, which include sands and gravels, occur where deposition is slow on the inner continental shelf and near the shelf edge. Those near the shelf edge include Last Glacial sandy muds that have been winnowed and mixed with Holocene volcanic ash and glauconite. The non‐detrital sediments, which contain forarninifera, volcanic ash, and glauconite, but no detrital sand, occur on anticlinal ridges on the continental slope. In places they overlie muddier sediment deposited during the last glaciation when the sources of river‐borne detritus were nearer than at present and when mud was deposited more rapidly on the ridges than at present. 相似文献
17.
不同养殖海域栉孔扇贝(Chlamys farreri)混合家系的通径分析 总被引：3，自引：0，他引：3
为了深入认识栉孔扇贝(Chlamys farreri)壳尺寸性状和体重之间的关系,达到通过直观可见形状判断非直观性状,在栉孔扇贝苗种培育中指导种贝挑选工作的目的,本实验将600余只扇贝分别于三个不同纬度养殖环境(山东青岛、山东荣成和辽宁大连)下养殖一年后测量其性状数据,包括壳长、壳高、壳宽、体重,进行壳尺寸性状对体重性状的通径分析。偏回归系数统计表明,除大连海域壳长对体重的偏回归系数为0.266,差异不显著(P0.05)外,其它参数对体重均极显著(P0.01),表明大多数自变量和因变量之间都有极显著的共线性关系。对各个海域建立以壳尺寸为自变量,体重为因变量的回归方程,得出通径系数、各性状间的相关性指数以及各参数对体重的决定系数,计算出了不同养殖地点的栉孔扇贝壳尺寸性状和体重之间关系的回归方程。通径分析显示,对青岛海域栉孔扇贝体重直接作用最大的是壳高,对荣成海域栉孔扇贝体重直接作用最大的是壳长,而对大连海域栉孔扇贝体重直接作用最大的是壳宽。因此,以体重为目标挑选青岛海域的种贝时,应以壳高为优先选择指标;挑选荣成海域的种贝时,优先选择壳长;挑选大连海域的种贝时,优先选择壳宽。不同养殖海域栉孔扇贝的通径分析为栉孔扇贝亲贝的挑选提供了理论支持。 相似文献
18.
不同贝龄毛蚶壳形态性状对体质量的影响 总被引：4，自引：0，他引：4
选取毛蚶(Scapharca subcrenata Lischke)1龄、2龄和3龄个体各100粒,分别测量壳长、壳高和壳宽等壳形态性状,并称其体质量,采用多元分析的方法分析了各表型性状间的相关性,以及壳形态性状对体质量的影响效果。结果表明,各性状间呈正相关,且达到极显著水平(P0.001);通径分析与决定程度分析的结果相似,不同贝龄期影响毛蚶体质量的主要因素是不同的,壳长是影响1龄毛蚶体质量的主要因素,壳长和壳宽是影响2龄毛蚶体质量的主要因素,且两者的共同决定系数最大(0.244),壳宽是影响3龄毛蚶体质量的主要因素,其与壳高的共同决定系数最大(0.230)。 相似文献
19.
Global warming and ocean acidification influence marine calcifying organisms, particularly those with external shells. Among these, mussels may compensate for environmental changes by phenotypic plasticity, but this may entail trade-offs between shell deposition, growth and reproduction. We assessed main and interactive effects of pH and temperature on four mussel species on the west coast of South Africa (33°48′ S, 18°27′ E) in October 2012 by comparing shell dissolution, shell growth, shell breaking force and condition index of two native species, the ribbed mussel Aulacomya atra and the black mussel Choromytilus meridionalis, and two aliens, the Mediterranean mussel Mytilus galloprovincialis and the bisexual mussel Semimytilus algosus. Live mussels and dead shells were exposed for 42 days to seawater of pH 7.5 or 8.0, at 14 °C or 20 °C. Low pH, high temperature and their combination increased shell dissolution of the two aliens but their growth rates and condition indices remained unchanged. Aulacomya atra also experienced greater shell dissolution at a low pH and high temperature, but grew faster in low-pH treatments. For C. meridionalis, shell dissolution was unaffected by pH or temperature; it also grew faster in low-pH treatments, but had a lower condition index in the higher temperature treatment. Shell strength was not determined by thickness alone. In most respects, all four species proved to be robust to short-term reduction of pH and elevation of temperature, but the native species compensated for greater shell dissolution at low pH by increasing growth rate, whereas the aliens did not, so their invasive success cannot be ascribed to benefits accruing from climate change. 相似文献
20.
In this paper the physical properties, chemical and mineral compositions of Huanghai glauconites are dealt with, and several factors associated with the growth of Huanghai glauconite are discussed, such as the type of bottom sediments, rate of sedimentation and the oxidation. Thus, a preliminary understanding of the growth of Huanghai glauconite is put forward. 相似文献