基于IDL的岛屿岸线及港口码头的人工智能提取

岛屿岸线的确定是海岛地物信息遥感调查中重要的一步,对舟山岙山岛的Quickbird高分辨率遥感影像进行地物地理信息分析,提取出岛屿岸线及港口码头的空间基本地物特征,在此基础上运用面向对象分类方法和数学形态学的知识,在ENVI＋IDL图形图像处理平台上实现对岛屿岸线及港口码头的自动提取,提取结果与实际情况基本符合,并且可以为人工智能提所有海岛地物信息的取做准备。     

Sipunculus nudus Linnaeus, 1766 (Sipuncula): cosmopolitan or a group of pseudo‐cryptic species? An integrated molecular and morphological approach

Sipunculan taxonomy relies on a limited set of external morphological and internal anatomical characters. In addition, this marine group is characterized by an unusual large number of putatively cosmopolitan species. However, this ‘cosmopolitan’ status could be an artifact of their conserved morphology and the small number of unambiguous taxonomic characters available for delimiting species. Species delimitation can therefore be aided by molecular techniques. We investigated the case of the widespread and common species Sipunculus nudus Linnaeus, 1766 to determine its systematic validity. We analysed the morphology of multiple specimens of S. nudus collected from 11 localities around the world and undertook phylogenetic analyses using molecular sequence data from four genes (28S rRNA, 16S rRNA, histone H3 and cytochrome c oxidase subunit I). High levels of genetic differentiation are present between distantly related populations of the putative species S. nudus. Five distinct lineages were identified by phylogenetic analyses, three of which – the best‐represented populations – can be distinguished morphologically. Our phylogenetic and morphological analyses thus do not favor the cosmopolitan status of S. nudus, suggesting instead that it constitutes a complex of morphologically similar but distinguishable species.     

Taxonomic description of a new marine ciliate,Euplotes qingdaoensis n. sp. (Ciliophora: Euplotida)

The characteristics and infraciliature of a new euplotid ciliate,Euplotes qingdaoensis n.sp.,discovered from the coastal waters of Jiaozhou Bay,northern China,were studied using live observation and silver impregnation.The new marine species is characterized by a slightly fl attened body(90–110 μm×70–80 μm,in vivo),an adoral zone of 26–29 membranelles,10 strong frontoventral and fi ve transverse cirri,two caudal cirri,a single left marginal cirrus,seven dorsal kineties,a middle kinety with about 15 pairs of basal bodies,a silverline system of the double-eurystomus type,and a C-shaped macronucleus.     

五种管口类纤毛虫的形态学研究

管口目纤毛虫由于个体微小且大部分种类缺乏现代分类学的研究,是纤毛门中较混乱的类群之一。为进一步了解其形态性状的种群间差异,借助显微活体观察及蛋白银染色法对采自青岛、湛江和香港近岸的斯雷腹沟虫(Coeloperix sleighi)、尖绒毛虫(Microxysma acutum)、乙状轮毛虫(Trochilia sigmoides)、阿氏直毛虫(Orthotrochilia agamalievi)和近岸类偏体虫(Agnathodysteria littoralis)5种管口类纤毛虫进行了形态学再研究,依据新采集种群,对其活体形态和纤毛图式特征进行补足性描述。结果发现,斯雷腹沟虫、乙状轮毛虫和阿氏直毛虫的形态性状极为稳定,而新采集的尖绒毛虫和近岸类偏体虫种群在伸缩泡数目上同前人描述略有差异。     

EDAPHIC LIMITATION OF A BRAZILIAN RAINFOREST PALM: THE ROLE OF ENERGY ALLOCATION AND COMPETITION FOR SUNLIGHT

Tropical forest palms are often associated with specific soil conditions, yet the ecological role of edaphic limitation in Palmae has seldom been considered. In the Atlantic Coastal Forest Biome of eastern Bahia, Brazil, the piassava palm (Attalea funifera) inhabits coastal podzolic soils but not nearby latosols. This paper examines the role of changing edaphic conditions and access to sunlight in the restriction of this species to tropical podzols.     

Clustering and classifying channel morphology in Eastern Oklahoma ecoregions using dissimilarity coefficients

Ecoregions are generally homogenous areas that comprise similar associations of geology, climate, soils, land use, and potential natural vegetation. However, a certain amount of physical variability exists in ecoregions which makes them spatially diverse in their characteristics. Euclidean Sum of Squares was used to calculate the amount of stream reach dissimilarity within and between three prominent eastern Oklahoma ecoregions: Boston Mountains, Ozark Highlands, and Ouachita Mountains. Dissimilarity proximity coefficients were used to cluster stream reaches and create exemplars for each cluster. Streams were classified using the Rosgen classification to evaluate whether dissimilarity values could be applied to the classification. Metrics used to calculate stream reach dissimilarity were median particle size, bankfull width, width–depth ratio, gradient, and sinuosity. Maximum stream reach dissimilarity between two sites within the same ecoregion is highest in the Ouachita Mountains (18.59) and followed by the Ozark Highlands (13.12) and Boston Mountains (9.58). Removal of ecoregion boundaries increased maximum proximity coefficient dissimilarity between two sites in the Ozark Highlands and Ouachita Mountains to 34.26. Utilizing the dissimilarity of channel morphology for the purpose of regional classification helps in the understanding of how broad-scale processes influence the fluvial system.     

Effects of Woody Debris on Channel Morphology and Sediment Storage in Headwater Streams in the Great Smoky Mountains,Tennessee-North Carolina

Coarse woody debris (CWD) is an important component of headwater streams, however, few studies have investigated the geomorphic effects of CWD in the southern Appalachians. In the Great Smoky Mountains, debris slides supply large volumes of CWD and sediment to low-order streams. This study investigates the effect of CWD on bankfull channel dimensions and in-channel sediment storage along second-order streams. Comparisons are made between streams that have experienced recent debris slides and those that have not. CWD channel obstructions are larger but less frequent along debris-slide-affected streams. Dendrochronological evidence indicates that CWD can remain in channels for over 100 yr. Relatively short residence times of CWD along debris-slide-affected streams suggest that logs are frequently flushed through these streams. CWD causes channel widening along all study streams, but the volume of sediment stored in the channel behind CWD obstructions is up to four times greater than the volume of sediment represented by bank erosion associated with CWD. Two large log jams formed by debris slides at tributary junctions stored approximately 4000 m³ of sediment. Sediment stored by CWD was finer than mean bed particle size, and thus represents a significant sediment source when CWD obstructions are breached.     

Fluvial diversity in relation to valley setting in the source region of the Yangtze and Yellow Rivers

The spatial distribution of valley setting （laterally-unconfined, partly-confined, or confined） and fluvial morphology in the source region of the Yangtze and Yellow Rivers is contrasted and analyzed. The source region of the Yangtze River is divided into 3 broad sections （I, II and III） based on valley setting and channel gradient, with the upstream and downstream sections being characterized by confined （some reaches partly-confined） valleys while the middle section is characterized with wide and shallow, laterally-unconfined valleys. Gorges are prominent in sections I and III, while braided channel patterns dominate section II. By contrast, the source region of the Yellow River is divided into 5 broad sections （sections I-V） based on valley characteristics and channel gradient. Sections I, II and IV are alluvial reaches with mainly laterally-unconfined （some short reaches partly-confined） valleys. Sections III and V are mainly confined or partly-confined. Greater morphological diversity is evident in the source region of the Yellow River relative to the upper Yangtze River. This includes braided, anabranching, anastomosing, meandering and straight alluvial patterns, with gorges in confined reaches. The macro-relief （elevation, gradient, aspect, valley alignment and confinement） of the region, linked directly to tectonic movement of the Qinghai-Tibet Plateau, tied to climatic, hydrologic and biotic considerations, are primary controls upon the patterns of river diversity in the region.     

Aggregatstabilitetsanalyse

Madsen, Henrik, 1975: Aggregatstabilitetsanalyse. Geografisk Tidsskrift 74: 70–78. København, juni 1, 1975.

A method to describe the stability and size distribution of soil aggregates by dry sifting. The profit and disadvantages of the method are discussed. A methematical adaption is given and further the influence of humus on the soil aggregates is discussed, as well as the possibility of the method for giving significant values in relation to soil erosion.