排序方式： 共有13条查询结果，搜索用时 15 毫秒
1.
Margarita Jambrina-Enríquez Clemente Recio Ildefonso Armenteros 《Environmental Earth Sciences》2018,77(2):49
The present multi-isotopic study (δ18O–δDwater, δ34S–δ18Odissolved-sulphate, δ13Cdissolved-inorganic-carbon, δ13C–δ18Oshells-modern-gastropods, δ13Cplants, and δ13Csedimentary-organic-matter) is aimed at assessing the hydrogeochemical changes and biogeochemical dynamics in a Mediterranean shallow lake fed by a Quaternary–Tertiary aquifer, the “Laguna del Cristo” (NW Iberian Peninsula), a system sensitive to climate fluctuations, between 2010 and 2011. Lake water is of the bicarbonate type, and there are no major pollutants. δ18O-δDwater values plot on a local evaporation line (δD=5.29δ18O–12.29) indicating that evaporative enrichment had a significant impact on lake water isotopic features. Periods of high water levels are characterized by lower δ34S–δ18Odissolved-sulphate and δ13Cdissolved-inorganic-carbon values and suggest sulphate derived from weathering of sulphides in the catchment area, delivered to the lake by surface run-off or via groundwater, and in situ decay of organic matter. During lower water levels, sulphate reduction and enhanced primary productivity lead to higher δ34Sdissolved-sulphate and δ13Cdissolved-inorganic-carbon values. Evaporation induced enrichment in 18Osulphate, 13Cdissolved-inorganic-carbon and 13C–18Oshells-Galba-Gyraulus. δ13Cplant confirms the C3 photosynthetic pathway. Enrichment in 13C submerged aquatic plants indicates that HCO3? is the main carbon source, except for 13C-depleted Potamogeton. The TOC, δ13Corg values, and TC/TN ratios in sediments all confirm the autochthonous character of organic matter contribution. This study provides a baseline for isotopic research into shallow, flow-through lakes fed by siliciclastic aquifers, and stresses the importance of evaporation and refilling (direct precipitation and groundwater discharge) in controlling the solute chemistry and stable isotopic composition in temperate regions with contrasting seasonal climates. The results also provide a snapshot of modern lake isotope variability that can be applied to paleoenvironmental reconstructions. 相似文献
2.
Biodiversity patterns of free-living marine nematodes in a tropical bay: Cienfuegos, Caribbean Sea 总被引：2，自引：0，他引：2
M. Armenteros A. Ruiz-Abierno R. Fernndez-Garcs J.A. Prez-García L. Díaz-Asencio M. Vincx W. Decraemer 《Estuarine, Coastal and Shelf Science》2009,85(2):179-189
Spatial and temporal biodiversity patterns of free-living marine nematodes were studied in Cienfuegos Bay, a tropical semi-enclosed basin in the Caribbean Sea. Taxonomic (to species level) and functional (biological trait) approaches were applied for describing the assemblage structure and relating it to abiotic environment based on a sampling scheme in six subtidal stations and three months. Biological trait approach added relevant information to species pattern regarding relationships between diversity patterns and the abiotic environment. The most common morphotypes were deposit feeding nematodes, with colonising abilities of 2–3 (in a scale from 1 to 5), tail conical cylindrical or filiforme and body slender; and their abundance were correlated with depth, organic matter and silt/clay fraction. In spite of a high turnover of species, functional diversity of assemblages did not change notably in space and time. A result probably due to sampling of the habitat pool of species and to low heterogeneity of the studied muddy bottoms. Chemical pollution (organic enrichment and heavy metals) and hydrodynamic regime possibly drove the biodiversity patterns. Spatial distribution of assemblages support the existence of two well differentiated basins inside the bay, the northern basin more polluted than the southern one. The low hydrodynamic regime would determine a poor dispersion of nematodes resulting in high spatial variance in the assemblage structure; and also the associated hypoxic conditions and pollutants in sediments can explain the dominance of tolerant nematode species such as Daptonema oxycerca, Sabatieria pulchra, Terschellingia gourbaultae, and Terschellingia longicaudata. A comparison of spatial–temporal patterns of biodiversity between Cienfuegos Bay and other semi-enclosed bays in temperate regions suggests several similarities: nematode assemblages are strongly influenced by anthropogenic disturbance, temporal trends are weak or overridden by spatial ones, and few cosmopolitan genera/species tolerant to pollution and hypoxic conditions are dominant. 相似文献
3.
4.
Linking sedimentation rates and large‐scale architecture for facies prediction in nonmarine basins (Paleogene,Almazán Basin,Spain) 
下载免费PDF全文
下载免费PDF全文 Luis Valero Pedro Huerta Miguel Garcés Ildefonso Armenteros Elisabet Beamud Miriam Gómez‐Paccard 《Basin Research》2017,29(Z1):213-232
This article focuses on the relationships between the large‐scale stratigraphic architecture of the Almazán basin infill and the sedimentation rates (SR) calculated for precise time intervals. Our aim was to improve the understanding of the timing and causes of the architectural changes, their significance in terms of accommodation space and sediment supply and their relationship with climate and tectonics. The study area includes the Gómara fluvial fan, the main sediment transfer system of the Almazán basin during Paleogene times. Its large‐scale architecture shifted through time between a stacking pattern of low density ribbon‐like and high density sheet‐like channel fills. Laterally to the fluvial system, mudstone and evaporitic mudstone units represented evaporitic mudflats which passed laterally into palustrine/lacustrine limestone units interpreted as lakes and ponds. Stacked calcretes occurred in distal alluvial and distal floodplain settings. A magnetostratigraphy encompassing 2600 m guided by available fossil mammal biochronology has provided a temporal framework that spans the complete Paleogene infill of the basin, from Late Lutetian to Late Oligocene, filling a gap in the Cenozoic chronostratigraphy of Spanish basins. This permits to constrain the kinematics of the structures both in the basin and in its margins, and to provide the timing for the depositional sequences. These data, combined with a magnetostratigraphic map, where magnetic reversals were traced through the Gómara monocline, allow a detailed analysis of the SR variability across the fluvial system and its adjacent depositional environments. The results show that high sedimentation rates (around 30–40 cm kyr?1) are related to fluvial environments with low density ribbon‐shaped channels, while low SR (around or below 10 cm kyr?1) are related to high density sheet‐like channels. Laterally, mud dominated environments with high SR (15–20 cm kyr?1) grade into palustrine/lacustrine carbonated environments with low SR (around 9 cm ky?1). The lowest SR (about 3 cm kyr?1) are related to the development of stacked calcrete profiles in distal floodplain and in the connection of distal alluvial and palustrine/lacustrine units. 相似文献
5.
M. Armenteros I. Martín J. P. Williams B. Creagh G. González-Sansón N. Capetillo 《Estuaries and Coasts》2006,29(1):124-132
The spatial and temporal variations of meiofaunal communities in mangrove systems were examined. Replicated cores were taken
in mudflats between prop roots ofRhizophora mangle at five locations within the Gulf of Batabanó, Cuba, during 3 mo. There was a clear seasonality in the water column, but
measured abiotic variables did not show obvious relations with meiofaunal patterns. The magnitude of change in salinity for
each location appears to influence the meiofauna more than absolute values per se. The meiofauna from southern Pinar del Rio
showed a higher variation in community structure, suggesting higher levels of stress in comparison with locations in eastern
Isla, possibly due to the presence of human settlements, runoff from land, and apparent deterioration of mangroves. The considerable
variation in the density and community structure estimates on global (geographical regions) and local (locations in the Gulf
of Batabanó) scales could be caused by the high spatial variability in the mangrove microenvironment, coupled with associated
methodological differences in the sampling. There was a low density of meiofauna (mean: 101 animals 10 cm−2) compared to other shallow tropical habitats. Mangroves from subtropical and temperate regions showed consistently higher
meiofaunal densities than tropical mangroves, but causes of this putatively latitudinal pattern require further study. Future
strategies for meiofaunal studies in mangrove systems should increase the temporal and spatial replication, include designed
field experiments to test ecological hypotheses, and apply a species level approach with regards to nematode assemblages. 相似文献
6.
Factors determining subsidence in urbanized floodplains: evidence from MT‐InSAR in Seville (southern Spain) 下载免费PDF全文
下载免费PDF全文 Ana Ruiz‐Constán Antonio M. Ruiz‐Armenteros Jesús Galindo‐Zaldívar Francisco Lamas‐Fernández Joaquim João Sousa Carlos Sanz de Galdeano Antonio Pedrera Sergio Martos‐Rosillo Miguel Caro Cuenca J. Manuel Delgado Ramon F. Hanssen Antonio J. Gil 《地球表面变化过程与地形》2017,42(14):2484-2497
Major rivers have traditionally been linked with important human settlements throughout history. The growth of cities over recent river deposits makes necessary the use of multidisciplinary approaches to characterize the evolution of drainage networks in urbanized areas. Since under‐consolidated fluvial sediments are especially sensitive to compaction, their spatial distribution, thickness, and mechanical behavior must be studied. Here, we report on subsidence in the city of Seville (Southern Spain) between 2003 and 2010, through the analysis of the results obtained with the Multi‐Temporal InSAR (MT‐InSAR) technique. In addition, the temporal evolution of the subsidence is correlated with the rainfall, the river water column and the piezometric level. Finally, we characterize the geotechnical parameters of the fluvial sediments and calculate the theoretical settlement in the most representative sectors. Deformation maps clearly indicate that the spatial extent of subsidence is controlled by the distribution of under‐consolidated fine‐grained fluvial sediments at heights comprised in the range of river level variation. This is clearly evident at the western margin of the river and the surroundings of its tributaries, and differs from rainfall results as consequence of the anthropic regulation of the river. On the other hand, this influence is not detected at the eastern margin due to the shallow presence of coarse‐grain consolidated sediments of different terrace levels. The derived results prove valuable for implementing urban planning strategies, and the InSAR technique can therefore be considered as a complementary tool to help unravel the subsidence tendency of cities located over under‐consolidated fluvial deposits. Copyright © 2017 John Wiley & Sons, Ltd. 相似文献
7.
8.
The EU accession countries have a high potential for low cost greenhouse gas emission reduction. As they cannot join the “bubble” agreement for the first commitment period of the Kyoto Protocol, project-based Joint Implementation (JI) could be a powerful strategy to integrate them into the EU climate policy strategy. An important question is whether the acquis communautaire will be used to define the baseline for the calculation of emission reductions from JI projects. A problem is that the grace periods for several environmental sectors differ considerably among countries. The EU should help accession countries to establish a predictable legal framework for JI preventing in this way the current legal uncertainty regarding JI procedures. 相似文献
9.
10.
Dolomitization,gypsum calcitization and silicification in carbonate–evaporite shallow lacustrine deposits 下载免费PDF全文
下载免费PDF全文 This paper describes and interprets the mineral and facies assemblages that occur in carbonate–evaporite shallow lacustrine deposits, considering the importance of the processes pathway (i.e. dolomitization, gypsum calcitization and silicification). The Palaeogene deposits of the Deza Formation (Almazán Basin, central‐northern Spain) are selected as a case study to determine the variety of physicochemical processes taking place in carbonate–evaporite shallow lakes and their resulting diagenetic features. Dolostones are the predominant lithology and are composed mainly of dolomite with variable amounts of secondary calcite (5 to 50%), which mainly mimic lenticular gypsum (pseudomorphs). Five morphological types of dolomite crystal were identified as follows: dolomite tubes, dolomite cylinders, rhombohedral dolomite, spheroidal and quasi‐rhombohedral dolomite, and cocoon‐shaped dolomite. The dolomite cylinders and tubes are interpreted as the dolomitized cells of a widespread microbial community. The sequence of diagenetic processes started with growth of microlenticular interstitial gypsum in a calcareous mud deposited on the playa margin mudflats, and that sometimes included microbial sediments. Immediately following growth of gypsum, dolomite replaced the original calcite (or possibly aragonite) muds, the microbial community and the gypsum. Partial or total replacement of gypsum by dolomite was related mainly to the biomineralization of endolithic microbial communities on gypsum crystals. Later calcitization took place under vadose, subaerial exposure conditions. The development of calcrete in distal alluvial settings favoured the release of silica and subsequent silicification on the playa margin mudflats. Stable isotope compositions of calcite range from ?9·02 to ?5·83‰ δ13CPDB and ?7·10 to 1·22‰ δ18OPDB; for the dolomite, these values vary from ?8·93 to ?3·96‰ δ13CPDB and ?5·53 to 2·4‰ δ18OPDB. Quartz from the cherts has δ18OSMOW values ranging from 27·1 to 31·1‰. Wide variation and relatively high δ18OSMOW values for dolomite indicate evaporitic and closed hydrological conditions; increased influx of meteoric waters reigned during the formation of secondary calcite spar. 相似文献