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In this report, we show that when ed is mutated, the expression level of Fmi in interommatidia cells is increased and similar to that in ommatidia cells. Furthermore, adult ed mutation eye shows rough phenotype and misrotated ommatidia.

在此篇论文,我们发现在ed突变的情况下,Fmi在小眼间细胞的表现量会上升,并提高至与小眼细胞的表现量相仿,而且ed突变的成虫复眼会变的不平整且具有错误转向的小眼存在。

Super Minimize - Hold down a minimized card and it will get even smaller.

更小 -按住一个最小化的卡片,它可以变的更小

Such kinds of information as small faults, bonanzas and stocks can be interpreted by these high resolution remote sensing data, which seem to be closely related to numerous metal deposits in normal cases. This method can therefore serve as a means in search for metallic deposits.

研究发现,小尺度范围一些典型蚀变信息及小节理、断裂、岩脉及小岩株多期次侵入相等在高分辨率遥感影像上具有独特反映,这些信息往往与矿床具有密切关系,以此信息进行遥感找矿分析,可为快速找矿提供一种重要方法。

Such a mesh point expansion curve to the actual business card printing and membership card making great advantage because mesh point expansion in General with the ink density by, the largest amplitude modulated net changes in the middle and the naked eye, so people can easily see that different (people on the most sensitive of South).

这样的网不面蔓延弧线给本质制卡和会员卡制息带来了很不小的劣势,因为网不面蔓延凡是随着油墨密度的增增而变不小,调幅网最不小改变爆发在洋间调上,所以人肉目可以很便当不离看不入不同。

Such a mesh point expansion curve to the actual business card printing comes with a great advantages because mesh point expansion in General with the ink density by, the largest amplitude modulated net changes in the middle and the naked eye, so people can easily see that different (people on the most sensitive of South).

这样的网不面蔓延弧线给本质制卡带来了很不小的劣势,因为网不面蔓延凡是随着油墨密度的增增而变不小,调幅网最不小改变爆发在洋间调上,所以人肉目可以很便当不离看不入不同。

Settlement characteristics are studied based on formula of suspended sediment settling velocity and previous research results. Results show that the suspended sediment flux quickly decreases from the Hangzhou Bay to the offshore area. Although the suspended sediments are primarily transported towards the offshore area, net transport towards the Hangzhou Bay is also found in the study area. The study area is basically located in hydrodynamic balance belt, and the suspended sediment transport is characteristics of reciprocating movement and small amount of net sediment discharge. The net suspended sediment transport is mainly controlled by average current transport, Stokes drift-induced transport and gravitational circulation transport. The advection transport effect gradually weakens and gravitational circulation transport evidently intensifies from Hangzhou Bay to the offshore area. Settling velocity of single particles is far smaller than that of floccules, so, influence of flocculation of suspended sediments must be taken into the consideration.

结果表明,研究区净悬沙通量自杭州湾内向外海迅速变小,悬沙总体由杭州湾向外海输运,但同时存在向杭州湾方向的净输沙;研究区基本处于水动力平衡带,悬沙输运具有往复搬运、净输沙量小的特点;平均流输运、Stokes漂移输运和垂向净环流输运是引起悬沙泥沙净输运的主要作用机制,自口门至外海,平流输运作用逐渐减弱,垂向净环流输沙在悬沙净输运中所占比例逐渐增加;舟山群岛海域既是杭州湾向东海输运泥沙的重要通道,也是东海沿岸流携带泥沙向南输运的过渡地带;研究区单颗粒泥沙沉降速度很小,远小于絮凝沉降速度,在研究本区悬沙沉降时必须考虑絮凝的影响。

The study area is basically located in hydrodynamic balance belt, and the suspended sediment transport is characteristics of reciprocating movement and small amount of net sediment discharge. The net suspended sediment transport is mainly controlled by average current transport, Stokes drift-induced transport and gravitational circulation transport. The advection transport effect gradually weakens and gravitational circulation transport evidently intensifies from Hangzhou Bay to the offshore area. Settling velocity of single particles is far smaller than that of floccules, so, influence of flocculation of suspended sediments must be taken into the consideration.Incipient velocity and transport flux of surface sediments are analyzed using formulas of incipient velocity and transport flux. Transport trend and controlling factors of surface sediments are studied by the method of grain size trend analysis.

结果表明,研究区净悬沙通量自杭州湾内向外海迅速变小,悬沙总体由杭州湾向外海输运,但同时存在向杭州湾方向的净输沙;研究区基本处于水动力平衡带,悬沙输运具有往复搬运、净输沙量小的特点;平均流输运、Stokes漂移输运和垂向净环流输运是引起悬沙泥沙净输运的主要作用机制,自口门至外海,平流输运作用逐渐减弱,垂向净环流输沙在悬沙净输运中所占比例逐渐增加;舟山群岛海域既是杭州湾向东海输运泥沙的重要通道,也是东海沿岸流携带泥沙向南输运的过渡地带;研究区单颗粒泥沙沉降速度很小,远小于絮凝沉降速度,在研究本区悬沙沉降时必须考虑絮凝的影响。

Spikelets laterally compressed, floret 1, rachilla extension absent; glumes absent; lemma ovate, hyaline, 1-veined, keeled, apex extended into a subulate cusplike awn; palea variable in size, frequently about 2/3 lemma length, broad, 2-toothed, keels extended into mucros.

小穗侧面压扁,小花1,小穗轴扩展无;颖片无;卵形,透明的外稃,1脉,翻转,顶延长成为一钻形的cusplike芒;内稃大小易变,经常大约2/3外稃长度,宽,2齿状,龙骨延伸进短尖头。

Leaves reduced upwards. Inflorescence branching, umbels compound, terminal on stem and branches; bracts entire, 2–3-lobed to pinnate or absent; rays 5–20, those of primary terminal umbel stout, spreading-ascending or diffuse; bracteoles similar to bracts or absent; umbellules 10–30-flowered.

叶向上变小花序分枝,复伞状花序,在茎和分枝上顶生;苞片全缘,2-3浅裂到羽状的或无;伞辐5-20,那些初级顶生伞形花序坚固的,平展上升的或铺散的;小苞片类似苞片或无;小伞形花序10-30开花。

Inflorescence branching, umbels compound, terminal; bracts mostly absent, occasionally 1–4, linear or similar to uppermost leaf; rays few, usually 5–15; bracteoles present, usually linear, entire, apex rarely lobed; umbellules usually many-flowered.

叶向上变小花序分枝,复伞状花序,顶生;苞片多数无的,偶有1-4,线形或类似于最上部的的叶;伞辐很少的,通常5-15;小苞片存在,通常线形,全缘,先端很少浅裂;小伞形花序通常多花的。

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