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Mm wide; follicles with a thick, fibrous mesocarp

肉质的花序轴,苞片卵形,约1毫米;花冠裂片约4毫米宽;蓇葖果具一厚,纤维状 37 Merrillanthus 驼峰藤属

Sepals without a mucro, outer flat; corolla blue, with a paler or white center I.

没有一短尖头的萼片,外部公寓;花冠蓝色,具一浅或白色中锋I。

Corolla campanulate, ca. 5 mm; pedicels ca. 7 mm; tubule of thecae ca.

花冠钟状,约5毫米;花梗约7毫米;囊约1毫米,具一短距的细管。

Shrublets erect, to 50 cm tall, pubescent or puberulent except for corolla and adaxial leaf surface.

直立的小灌木,在50厘米高,具短柔毛或微柔毛除了花冠和叶正面。

Corolla campanulate , often bearded at mouth, tube short to long, lobes exduplicate-valvate in bud.

花冠钟状,在嘴具髯毛的通常,筒部短到长,在芽中裂片exduplicate有阀门。

Stamens 4, ascending beneath upper corolla lip; filaments complanate, puberulent; anthers with 2-locular, bearded pollen sacs.

雄蕊4,在上面花冠唇下面上升;花丝扁平,被微柔毛;花药具2室,具髯毛的花粉囊。

Corolla rotate, lobes longer than tube; seed coat smooth or with a denticulate margin .

花冠旋转,裂片长于筒部;种子给平滑的或涂上一具小齿边缘。

Stamens 4 and didynamous or 5, inserted high in corolla tube; anthers divergent, ellipsoid, longitudinally dehiscing, apex with a caudate appendage.

雄蕊4 和二强雄蕊或5,在花冠筒内着生高;花药分叉,椭圆形,纵向开裂,先端具一尾状的附属物。

Peduncles less than 2 cm, much shorter than leaves; leaf blade with lateral veins obscure or up to 6 pairs; corona lobes dorsiventrally compressed.

花序梗少于2厘米,远短于叶;叶片具侧脉不明显或可达6 对;背面的副花冠裂片压扁。

Stamens inserted at middle of corolla tube, with exserted long filaments and linear-oblong anthers.

雄蕊着生在中部的花冠筒,具长花丝和线状长圆形花药。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。