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干旱草甸
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     On resaerch ,We find that the four types of Xerophyte have typical structural features in adjusting to the arid envirement:short ,small leaves ,thick cuticle, developed surrounding paling tissues,developed chloroplast inside paling tissues,etc.
     对分布于吉林省西部干旱草甸上 4种旱生植物茎和叶的解剖学研究发现 ,它们具有适应旱生环境的典型结构特征 :植株矮、叶面积小、表皮细胞厚且有较厚的角质层 . 栅栏组织发达并具环栅结构、栅栏细胞内叶绿体发达等 .
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     and Ⅷ. Meadow.
     Ⅷ、草甸
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     (3)heavy drought number has increased ;
     (3)干旱增强;
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     Research On Drought Concept
     干旱概念探讨
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     Therefore, it is concluded that cultivation of meadow promoted the emissions of CO2. It was also found that the drought in 2001 cut the emissions of CO2 down seriously.
     另外干旱使得草甸草原、农田和休耕地的CO2排放量表现出减少趋势。
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     Responses of NPP of salinized meadow in hyper-arid area to global change
     极端干旱气候下盐化草甸植被净初级生产力对全球变化的响应
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After the investigation of the plants in Xianghai,we have gathered 59 families 152 genera and 208 species of angiosperm.The plants here are devided into 4 types,dry grassy marshland,low humid grassy marshland,hydrophyte,and sparse woods and bushes in sand dunes.

本文对向海自然保护区植物种类进行了调查 ,共采集被子植物 59科 1 52属 2 0 8种 .该保护区植被分四种类型 :干旱草甸、低湿草甸、水生植被、沙丘坨甸蔬林灌丛 .

On resaerch ,We find that the four types of Xerophyte have typical structural features in adjusting to the arid envirement:short ,small leaves ,thick cuticle, developed surrounding paling tissues,developed chloroplast inside paling tissues,etc. Out of their leaves and veins there are surrounding bundle sheath and large amount of villi.There are as well developed conducting tissues in the stems.

对分布于吉林省西部干旱草甸上 4种旱生植物茎和叶的解剖学研究发现 ,它们具有适应旱生环境的典型结构特征 :植株矮、叶面积小、表皮细胞厚且有较厚的角质层 .栅栏组织发达并具环栅结构、栅栏细胞内叶绿体发达等 .叶脉外有维管束鞘包围 ,而且叶有大量的表皮毛 .茎中导水组织发达

The south margin of Song-Liao basin is mostly covered by Quaternary strata with various types of origin. Based on their origin types, the Holocene strata distributed in Siping-Shuangliao area can be divided into following units: 1) the Wenquanhe formation of alluvial origin in early-middle epoch; 2) the Tantu formation of limnetic accumulation origin in the middle epoch; 3) the Daliaohe formation of alluvial origin in late epoch; 4) the Horqin formation of eolian accumulation origin; and 5) the Xieriga formation...

The south margin of Song-Liao basin is mostly covered by Quaternary strata with various types of origin. Based on their origin types, the Holocene strata distributed in Siping-Shuangliao area can be divided into following units: 1) the Wenquanhe formation of alluvial origin in early-middle epoch; 2) the Tantu formation of limnetic accumulation origin in the middle epoch; 3) the Daliaohe formation of alluvial origin in late epoch; 4) the Horqin formation of eolian accumulation origin; and 5) the Xieriga formation of limnetic accumulation origin. The early and middle Holocene epoch was in an environment of relative warm and humid veld to arid meadow vegetation; while the late epoch was in warm and humid veld to relative arid meadow vegetation environment.

松辽盆地南缘大面积被多种成因类型的第四系地层覆盖.按其成因类型,四平-双辽地区可划分的全新统地层单位有:早-中期冲积成因温泉河组;中期湖沼堆积成因坦途组;晚期冲积成因大辽河组;风积成因科尔沁组;湖沼堆积成因协日嘎组.全新世早-中期是一种比较温湿疏林草原—干早的草甸草原植被环境,晚期是一种温湿疏林草原—比较干旱的草甸草原植被环境.

 
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