第四纪研究
第四紀研究
제사기연구
2010年
2期
364-371
,共8页
杨晓燕%孔昭宸%刘长江%葛全胜
楊曉燕%孔昭宸%劉長江%葛全勝
양효연%공소신%류장강%갈전성
粟、黍及其近缘野生种%淀粉粒形态%中国北方
粟、黍及其近緣野生種%澱粉粒形態%中國北方
속、서급기근연야생충%정분립형태%중국북방
millets and their wild relatives%starch grain analysis%identification%North China
对来自中国北方不同区域的9个粟(Setaria italica)样品及其野生祖本青狗尾草(Setaria viridis)的7个样品,9个黍(Panicum miliaceum)样品及其近缘野生种糠稷(Panicum bisulcatum)和野黍(Eriochloa villosa)样本各 1个,共27个样品进行了淀粉粒分析.针对每个样品,统计 100~200颗淀粉粒粒径数据,100颗形态特征数据,在此基础上初步明确了5种植物淀粉粒如下判别特征: 1)5种淀粉粒中,除野黍淀粉粒为小粒径((X)=4.8±0.8μm)的椭球形和球形外,其余4种淀粉粒都以多面体为主,球形或近球形为辅,脐点居中开放,黍、粟、青狗尾草和糠稷淀粉的平均粒径分别为(X)=7.3±1.4μm,(X)=9.9±2.3μm,(X)=7.7±1.4μm和(X)=6.9±1.2μm.2)粒径大于12μm的淀粉粒一般不是黍的淀粉粒.3)粒径大于14μm的淀粉粒99.9%来自粟.3)粒径小于11μm的淀粉粒,如果超过40%的淀粉粒表面无裂隙,极有可能为黍属的淀粉粒; 如果有超过30%的淀粉粒表面具有裂隙,则非常有可能来自狗尾草属.4)近乎45%的粟淀粉粒粒径处于 11~14μm,而只有约4%的青狗尾草淀粉粒粒径位于这一区间.如果粒径在 11~14μm的淀粉粒含量超过获得淀粉粒总量的4% ,则其中很可能包含有粟的淀粉粒.以上标准在鉴定时还需要综合考虑.高粱(Sorghum bicolor)与薏米(Coix chinensis)在粒径和形态上与狗尾草属和黍属有部分重合,但大部分高粱的淀粉粒具有层纹,薏米则有30%的粒径大于14μm,与粟只有5%的淀粉粒位于这一粒径范围有很大的区别.通过研究发现,在现阶段,典型黍亚科(Panicoideae)种类淀粉形态在统计上的区别是明显的,但仅依靠少量颗粒特征进行区分是困难的,如何把现代淀粉特征准确应用到考古样品的鉴定中,还有待更多的淀粉埋藏学研究.目前,针对粟、黍及其野生近缘种的鉴别,植硅体分析的效果明显好于淀粉粒分析.
對來自中國北方不同區域的9箇粟(Setaria italica)樣品及其野生祖本青狗尾草(Setaria viridis)的7箇樣品,9箇黍(Panicum miliaceum)樣品及其近緣野生種糠稷(Panicum bisulcatum)和野黍(Eriochloa villosa)樣本各 1箇,共27箇樣品進行瞭澱粉粒分析.針對每箇樣品,統計 100~200顆澱粉粒粒徑數據,100顆形態特徵數據,在此基礎上初步明確瞭5種植物澱粉粒如下判彆特徵: 1)5種澱粉粒中,除野黍澱粉粒為小粒徑((X)=4.8±0.8μm)的橢毬形和毬形外,其餘4種澱粉粒都以多麵體為主,毬形或近毬形為輔,臍點居中開放,黍、粟、青狗尾草和糠稷澱粉的平均粒徑分彆為(X)=7.3±1.4μm,(X)=9.9±2.3μm,(X)=7.7±1.4μm和(X)=6.9±1.2μm.2)粒徑大于12μm的澱粉粒一般不是黍的澱粉粒.3)粒徑大于14μm的澱粉粒99.9%來自粟.3)粒徑小于11μm的澱粉粒,如果超過40%的澱粉粒錶麵無裂隙,極有可能為黍屬的澱粉粒; 如果有超過30%的澱粉粒錶麵具有裂隙,則非常有可能來自狗尾草屬.4)近乎45%的粟澱粉粒粒徑處于 11~14μm,而隻有約4%的青狗尾草澱粉粒粒徑位于這一區間.如果粒徑在 11~14μm的澱粉粒含量超過穫得澱粉粒總量的4% ,則其中很可能包含有粟的澱粉粒.以上標準在鑒定時還需要綜閤攷慮.高粱(Sorghum bicolor)與薏米(Coix chinensis)在粒徑和形態上與狗尾草屬和黍屬有部分重閤,但大部分高粱的澱粉粒具有層紋,薏米則有30%的粒徑大于14μm,與粟隻有5%的澱粉粒位于這一粒徑範圍有很大的區彆.通過研究髮現,在現階段,典型黍亞科(Panicoideae)種類澱粉形態在統計上的區彆是明顯的,但僅依靠少量顆粒特徵進行區分是睏難的,如何把現代澱粉特徵準確應用到攷古樣品的鑒定中,還有待更多的澱粉埋藏學研究.目前,針對粟、黍及其野生近緣種的鑒彆,植硅體分析的效果明顯好于澱粉粒分析.
대래자중국북방불동구역적9개속(Setaria italica)양품급기야생조본청구미초(Setaria viridis)적7개양품,9개서(Panicum miliaceum)양품급기근연야생충강직(Panicum bisulcatum)화야서(Eriochloa villosa)양본각 1개,공27개양품진행료정분립분석.침대매개양품,통계 100~200과정분립립경수거,100과형태특정수거,재차기출상초보명학료5충식물정분립여하판별특정: 1)5충정분립중,제야서정분립위소립경((X)=4.8±0.8μm)적타구형화구형외,기여4충정분립도이다면체위주,구형혹근구형위보,제점거중개방,서、속、청구미초화강직정분적평균립경분별위(X)=7.3±1.4μm,(X)=9.9±2.3μm,(X)=7.7±1.4μm화(X)=6.9±1.2μm.2)립경대우12μm적정분립일반불시서적정분립.3)립경대우14μm적정분립99.9%래자속.3)립경소우11μm적정분립,여과초과40%적정분립표면무렬극,겁유가능위서속적정분립; 여과유초과30%적정분립표면구유렬극,칙비상유가능래자구미초속.4)근호45%적속정분립립경처우 11~14μm,이지유약4%적청구미초정분립립경위우저일구간.여과립경재 11~14μm적정분립함량초과획득정분립총량적4% ,칙기중흔가능포함유속적정분립.이상표준재감정시환수요종합고필.고량(Sorghum bicolor)여의미(Coix chinensis)재립경화형태상여구미초속화서속유부분중합,단대부분고량적정분립구유층문,의미칙유30%적립경대우14μm,여속지유5%적정분립위우저일립경범위유흔대적구별.통과연구발현,재현계단,전형서아과(Panicoideae)충류정분형태재통계상적구별시명현적,단부의고소량과립특정진행구분시곤난적,여하파현대정분특정준학응용도고고양품적감정중,환유대경다적정분매장학연구.목전,침대속、서급기야생근연충적감별,식규체분석적효과명현호우정분립분석.
Following spore-pollen and phytolith analyses,starch grain analysis is a new approach to studying of paleoenvironmental reconstruction,plant-use history,agriculture origins,and historic land-use. In order to study the origin of dry-farming in North China,we collected 9 samples of foxtail millet(Setaria italica),7 samples of green foxtail grass(Setaria viridis),and 9 samples of broomcorn millets(Panicum miliaceum)and 2 samples of its wild relatives Panicum bisulcatum and Eriochloa villosa,one for each relative,from different regions in North China and analyzed their starch grain morphological characteristics. Both sizes of 100~200 starch grains and morphological characteristics of 100 starch grains were measured for each sample. Except that starch grains of Eriochloa villosa are spherical or ellipsoidal and smaller in grain size,4.8±0.8μm,starch grains of other four species are mainly polyhedric and have centric and open hila. For green foxtail grass,which is considered as the ancestor of foxtail millet,the starch grains are 7.7±1.4μm in the mean size and 14.0μm in the largest size,with 95% confidence interval(CI)being 7.6~7.9μm,and have slight fissures through their hila,rough edges,and wrinkled surfaces. For foxtail millet,the starch grains are 9.9±2.3μm in the mean size and 19.5μm in the largest,with 95%CI being 9.7~10.0μm,and have smooth surfaces,deep fissures and short lines radiating from centre to edge. For broomcorn millet,the starch grains are 7.3±1.4μm in the mean size and 11.9μm in the largest,with 95% CI being 7.2~7.4μm; 70% of them have not fissures through hila,which is an apparent difference from those two species of Setaria genus. For Panicum bisulcatum,which is considered as one candidate of the ancestor of broomcorn millet,the starch grains are very similar to those of broomcorn millet and 6.9±1.2μm in the mean size,with 95% CI being 6.7~7.1μm,but more than 30% of them have deep surface fissures. Based on the above statistical characteristics of starch grains,the following diagnostic criterions can be set up: 1)starch grains more than 12μm in size are generally not of broomcorn millet; 2)starch grains more than 14μm in size are generally of foxtail millet; 3)starch grains smaller than 12μm in size might be either of broomcorn millet if they have over 40% grains without fissures or of either foxtail millet or green foxtail grass if they have over 30% grains with fissures; and 4)because almost 45% starch grains of foxtail millet are 11~14μm in size,but only about 4% starch grains of green foxtail grass are in this size zone,if more than 4% starch grains are 11~14μm in size,some of them are surely of foxtail millet. In addition,if starch grains have deep fissure and smooth surfaces with radiating short lines,they may perhaps be of foxtail millet. If the starch grains have slight fissures,coarse edges,and winkled surfaces,they may perhaps be of green foxtail grass. We think that to identify millets and their wild relatives,starch grain analysis is not very more effective than phytolith analysis so far.