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41.
设施种植的主要气象灾害有低温(冷冻害)、寡照、风灾、雪灾及其复合灾害等,从国内设施种植气象灾害指标、灾害监测预警、灾害风险及灾害影响等方面对前人研究成果和进展进行归纳总结。灾害指标的研究所采用的方法主要是人工控制试验或对历年实际发生的灾害样本进行分析总结;灾害监测预警方法一般是用设施内小气候或设施外气象条件作为灾害指标,将灾害指标植入计算机系统,对灾害进行监测预警;风险评估多是从灾害的危险性角度去研究,确定灾害的风险概率、风险指数等;灾害影响的研究多集中在对作物生理生态反应等方面。同时从设施种植气象灾害研究存在的薄弱环节出发,提出设施种植气象灾害指标、灾害监测预警评估方法及灾害的影响等方面仍是今后一段时间研究的重点和热点。 相似文献
42.
栉孔扇贝♀×华贵栉孔扇贝♂受精及早期胚胎发育过程的细胞学荧光显微观察 总被引:4,自引:0,他引:4
为探讨贝类杂交优势 ,利用HOECHST3 3 2 5 8对已固定样品进行染色的方法 ,连续观察了栉孔扇贝♀×华贵栉孔扇贝♂受精的细胞生物学过程 ,初步证明了这 2种远缘扇贝种类之间进行杂交的可行性。结果表明 ,栉孔扇贝的成熟未受精卵子处于第一次减数分裂中前期 ,部分来自华贵栉孔扇贝的异源精子可顺利进入卵子并激发后者完成 2次减数分裂 ,排出第一及第二极体。成熟的雌雄原核形成后完成融合过程 ,形成合子核 ,受精过程结束。大部分杂交受精卵及杂种早期胚胎可以正常发育 ,但其发育进程较种内近交对照组有明显的差别 ,具体表现在延缓性和不同步性 2个方面。 相似文献
43.
44.
气候转型与早期人类迁徙 总被引:4,自引:0,他引:4
目前的旧石器考古证据表明,更新世早期可能发生了两次人类迁徙浪潮,时间分别在1.8-1.6MaBP和1.0MaBP左右,第一阶段,古人类演化为直立人并开始走出非洲、迁徙至其它中低纬度的热带-亚热带地区;第二阶段,直立人开始占据中高纬度的温带和干旱-半干旱地区。这两个阶段也是第四纪气候发生转型、环境产生重大调整的时期。二者在发生时间上的一致性揭示了它们之间的内在联系,推测气候转型时期环境转变是这两次人类迁徙浪潮的主要驱动力。 相似文献
45.
冬至初春黄海暖流的路径和起源 总被引:18,自引:0,他引:18
主要根据近几年来中韩黄海水循环动力学合作调查结果,结合有关观测资料,进一步分析了冬至初春黄海暖流的路径和起源.与以往类似研究不同的主要有两点:(1)初步探讨了黄海暖流路径的季节和年际变异,并指出这种变异与北向风的强弱密切相关;(2)通过分析济州岛西侧海域混合水的去向,进一步确认了部分混合水绕济州岛运行,并进入济州海峡这一事实.同时,初步揭示进入黄海的混合水,即黄海暖流水,含有更多的东海陆架水成分. 相似文献
46.
Spatial and seasonal variations in depth profile of trace metals in saltmarsh sediments from Sapelo Island, Georgia, USA 总被引:1,自引:0,他引:1
This study was undertaken to elucidate the impact of early diagenetic processes on the accumulation of trace metals in Sapelo Island saltmarsh sediments as a function of time, space and sediment properties. Samples were collected from three sites in summer (May 1997) and winter (January 1998) along a transect from an unvegetated Creek Bank through a vegetated Tidal Levee to the vegetated midmarsh with evident lateral heterogeneity caused by hydrologic regime, macrophytes and microbial and macrofaunal activities. A suite of trace metals (As, Ba, Cr, Co, Cu, Cd, Mo, Ni, Pb, Th, Ti, U, V, Zn and Zr) was analyzed to obtain their depth-distribution at the three sites. Spatially marked differences were observed, that were primarily related to hydraulic flushing of trace metals away from the sites in high-energy regimes, rapid downward mixing and reworking of sediment via bioturbation, and below-ground degradation and production of Spartina biomass. Although sulfate reduction and the formation of acid volatile sulfide and pyrite were dominant processes throughout the marsh, the trace metal scavenging role of sulfides was not apparent. However, possible sulfurization of organic matter, leading to enhanced trapping of trace metals with organic carbon, may have played an important role in sequestration of trace metals.No similarity was observed visually between the depth trends of trace metals and sediment properties (grain size, iron-oxyhydroxide content, acid volatile sulfides and pyrite content) that are known to play a major role in trace metal partitioning. Only organic carbon content closely followed the trace metal profiles at all the three sites. Minor variation in depth-integrated sediment trace metal content was observed seasonally at each of the three sites. Furthermore, the depth trend of profiles of individual trace metals also did not vary significantly over the seasons either. 相似文献
47.
滇中地区早前寒武纪地质研究新进展 总被引:1,自引:1,他引:0
滇中地区中元古界"昆阳群"的地层层序是长期争议的重大基础地质问题,在一定程度上制约了地质调查工作的部署及勘查效果,也制约着滇中地区前寒武纪地质研究水平的进一步提高。云南省地质调查院在进行《云南省区域地质志》(第二版、修编)、1:5万二街等4幅区域调查子项目工作中,在前人工作成果的基础上,通过大量的野外地质调查及锆石同位素年代学研究,在滇中地区早前寒武纪地层层序及时代、重大地质事件记录、早期生命与环境协同演化等方面取得了一系列的新发现,具有重要意义。 相似文献
48.
笔者于西藏仲巴县塔惹增地区一带前人划分的一套早白垩世早期则弄群中发现了具有典型意义的、代表早白垩世晚期的Ampullina xainzaensis Yu,Ampullina cf. larteli Landerer,Tylostoma cf. brasilianus Maury,Pseudamaura cf. subfournaeti (Pcelincev),Gyrodes gaultiana Orbigny,Leviathania cf. gerassimovi(Pcelincev),Gymnentome cf. pizcuetana(Vilanova)等腹足类化石,以及较为丰富的中圆笠虫Mesorbitolina sp.和达克斯虫Daxia sp。表明在该区则弄群中至少有一部分以前没有被识别出的早白垩世晚期地层。通过岩石组合特征、基本层序、生物化石时代对比,将该套地层归属于捷嘎组。这一地层的确定为冈底斯带白垩系地层划分对比、地层格架建立提供了重要的依据,并丰富了该地层的古生物资料,且为中生代盆地的演化历史、古地理轮廓的确定提供了新的基础资料。 相似文献
49.
The remarkable transition of early angiosperms from a small to a dominant group characterized the terrestrial ecosystem of the Cretaceous. This transition was instigated and promoted by environmental changes. Mid-Cretaceous is characterized by major geological events that affected the global environment. δ18O, palaeothermometer TEX86, and other climatic indices from marine sediments suggest rapid temperature increase during mid-Cretaceous despite occasional short cooling events. Simultaneously, terrestrial deposits in East Asia changed from coal-bearing to shale, then to red beds and evaporites. Plant assemblages and other paleoclimate indicators point to rapid aridification for mid-Cretaceous terrestrial environments. In addition, the wildfires were frequently spread all over the earth by the numerous charcoal evidence during the Mid-Cretaceous. Thus, we speculate that the seasonally dry and hot conditions of mid-Cretaceous created a fiery hothouse world. Early angiosperms increased in abundance and diversity and evolved from a few aquatic species to terrestrial herbaceous and then to the diversified flora of today. Angiosperms showed rapid physiological evolution in vein density and leaf area that improved photosynthesis and water absorption. These ecophysiological changes made early angiosperms well adapted to the hot and dry environment in mid-Cretaceous. Moreover, these physiological changes facilitated the fire–angiosperm cycles in mid-Cretaceous that likely further stimulated the early angiosperm evolution. 相似文献
50.
Tian-Yu Zhang Cai Li Chao-Ming Xie Ming Wang Yan-Wang Wu 《International Geology Review》2018,60(4):449-463
Zircon U–Pb dating of two samples of metagabbro from the Riwanchaka ophiolite yielded early Carboniferous ages of 354.4 ± 2.3 Ma and 356.7 ± 1.9 Ma. Their positive zircon εHf(t) values (+7.9 to +9.9) indicate that these rocks were derived from a relatively depleted mantle. The metagabbros can be considered as two types: R1 and R2. Both types are tholeiitic, with depletion of high-field-strength elements (HFSE) and enrichment of large-ion lithophile elements (LILE) similar to those of typical back-arc basin basalts (BABB), such as Mariana BABB and East Scotia Ridge BABB. Geochemical and isotopic characteristics indicate that the R1 metagabbro originated from a back-arc basin spreading ridge with addition of slab-derived fluids, whereas the R2 metagabbro was derived from a back-arc basin mantle source, with involvement of melts and fluids from subducted ocean crust. The Riwanchaka ophiolite exhibits both mid-ocean ridge basalts- and arc-like geochemical affinities, consistent with coeval ophiolites from central Qiangtang. Observations indicate that the Qiangtang ophiolites developed during the Late Devonian–early Carboniferous (D3–C1) in a back-arc spreading ridge above an intra-oceanic subduction zone. Based on our data and previous studies, we propose that an oceanic back-arc basin system existed in the Longmuco–Shuanghu–Lancang Palaeo-Tethys Ocean during the D3–C1 period. 相似文献