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茎状

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Leaf blade linear-lanceolate, bullate, margin revolute, entire; fruit reddish, punctate-lineate, wrinkled

叶片线形披针形,具泡状隆起,边缘外卷,全缘;果带红色,具点有线,起皱 19 Maesa salicifolia 柳叶杜茎山

Shrubs or trees, deciduous or evergreen, often from underground woody burl or producing thickened horizontal underground rhizomes.

灌木或乔木,落叶或常绿,通常生于地下木质瘤或产加厚的水平的地下根状茎。

Leaf blade membranous, elliptic to ovate, margin serrate, teeth not callose; inflorescences 7-10 cm, racemose

叶片膜质,椭圆形到卵形,边缘有锯齿,齿而不是callose;花序7-10厘米,总状 27 Maesa tenera 软弱杜茎山

Stem absent; panicle, similar to spike or capitulum; stamens subequal to perianth.

茎无; 圆锥花序,类似于穗状花序或小头花状序;雄蕊近等长于花被。

Herbs perennial, scapose, rhizomatous or with a caudex covered with petiolar remains of previous years.

多年生草本,具花葶,根状茎或具一为petiolar所覆盖残余的第二年。

Rhizome a fleshy caudex, thick or slender, apex usually at or slightly above ground level.

根状茎一肉质块根,纤细的厚或,先端通常在或稍高于地面。

Herbs perennial, rhizomatous or with a caudex.

多年生草本,根状茎或具一块根。

Base of vegetative stems forming a stout caudex; leaves and calyx lobes with white cartilaginous margin and midrib keel.

营养体茎的基部形成一粗壮块根;叶和萼裂片具白色的软骨质的边缘和中脉龙骨状。

Big leaf area could increase photosynthetic product;Less scourgelike caudex differentiation makes accumulation of corm material more efficient.

在花魔芋生长期间发现了大叶片植株、耐寒植株、少鞭状茎分化植株和高球茎增重系数植株等有益突变。

Hybrids of carbonate and terrigenous sediments Carbonate with terrigenous sediments are of characteristic from Emsian to Eifelian in stable shallow-sea faciesregion in Longmenshan area, and they can be classified evidently into hybrid Ⅰ and hybrid Ⅱ(Jingbaoshi-type). Type Ⅰ produced in mud shelf setting occupied hundreds of tempestite beds in which bottom cast、 hummocky cross bedding sandstones、 coquina were inter-beddded with shales that beared a great deal of verm traces、 bioturbations、 benthic communities dominative of brachiopods. Type Ⅱ in sand-mud-marl shelf was characterized by high-energy foreshore sandbeach facies and shelly bank facies.

碳酸盐与陆源碎屑混合沉积方面对微相、相特征、旋回样式、沉积机理研究表明,龙门山地区泥盆纪稳定浅海相区Emsian期和Eifelian期混合沉积十分发育,颇具特色,明显可以划分为两种类型:混积Ⅰ型,泥质陆棚背景下发育风暴沉积组构,幕式风暴期产生具丘状层理、底流冲刷构造的钙质砂岩、介壳岩,平息期则形成具大量虫管和生物扰动的深灰色、黄绿色页岩及海百合茎灰岩,腕足动物等大量繁盛;混积Ⅱ型,砂泥灰质陆棚背景下以发育高能前滨沙滩及生物介屑滩为特色,近滨至陆棚的砂泥灰互为混合,三者比例接近,肉眼难以区别确切岩石类型。

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