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More active air, a matutinal distant cock, ecclesiastical clocks at various points, avine music, the isolated tread of an early wayfarer, the visible diffusion of the light of an invisible luminous body, the first golden limb of the resurgent sun perceptible low on the horizon.

406空气越发充满了勃勃生机:远处,公鸡在报晓,各座教堂的敲钟声,鸟类的音乐,早起的行人那孤零零的脚步声,看不见的光体所射出的看得见的光,复活了的太阳那低低地崭露在地平线上的、依稀可辨的最初一抹金晖。

It was a major regional focal point in the northern Maya lowlands from the Late Classic through the Terminal Classic and into the early portion of the Early Postclassic period. The site exhibits a multitude of architectural styles, from what is called "Mexicanized" and reminiscent of styles seen in central Mexico to the Puuc style found among the Puuc Maya of the northern lowlands.

它是玛雅低地从晚古典时期经过最终古典进入后古典时期早期的一个主要的地区焦点,该遗址展现了许多建筑风格,从所谓的"墨西哥式"和中部墨西哥的怀旧风格到北部低地普克玛雅中发现的普克风格,风格各异,多姿多彩。

West Low German is a general term for a series of Low German dialects, located in northwest Germany, the Netherlands East ...

西低地德语是一系列低地德语方言的总称,分布于德国西北部、荷兰东部。。。。

East Low German is a general term for a series of Low German dialects, located in northeastern Germany, the Polish minority in northern areas.

低地德语是一系列低地德语方言的总称,分布于德国东北部、波兰北部的少数族裔区。

Above the high tidal flat and lowland strata of MIS 3, the marine microfossils continuously or discontinuously occur at some horizons of estuary facies and neighbor lowland, even during the Last Glacial Maximum, but only of the euryhaline and low-salinity assemblages generally, which do not extend far from the paleo-river.

在MIS3阶段高潮坪一低地沉积之后,河口与相邻低地依然持续或断续出现海相微体生物,个别钻孔中其分布甚至延续到末次盛冰期低海面地层中,但是基本都是广盐种和低盐种。

Above the high tidal flat and lowland strata of MIS 3,the marine microfossils continuously or discontinuously occur at some horizons of estuary facies and neighbor lowland,even during the Last Glacial Maximum,but only of the euryhaline and low-salinity assemblages generally,which do not extend far from the paleo-river.

在MIS3阶段高潮坪-低地沉积之后,河口与相邻低地依然持续或断续出现海相微体生物,个别钻孔中其分布甚至延续到末次盛冰期低海面地层中,但是基本都是广盐种和低盐种。

As the last Wisconsin glacier retreated,postglacial lakes were formed in the southeastern and northwestern parts of the Hudson Lowland(including the southern part of James Bay Lowland)with stratified silt and sand deposited over the upper till.

作为最后威斯康星冰川后退,后期形成的湖泊在东南部和西北部地区的哈德逊低地(包括南部的詹姆斯湾低地)分层淤泥和沙子沉积在上游到。

From 6860 to 3170 cal.yr BP,semi-desert steppeexpanded,regional montane forest steppe retreated,suggesting a prolonged warm and dryclimate.Between 3170 and 2340 cal.yr BP,regional forest steppe expanded whereassemi-desert steppe retreated,indicating the climate became cool and wet gradually and thehumidity reached the maximum at the end of this stage.During 2340~1600 cal.yr BP,Poaceae steppe dominated whereas wetland meadow expanded and the montane forest stepperetreated,suggesting a cool and wet climate prevailed,wormwood grass steppe prevailed andthe climatic instability increased after 1600 cal.a BEThe climate and environmental reconstructions by pollen were supported by the diatomrecords.A relative high lake level and moister climate prevailed between 8660 and 7230 cal.yr BP as inferred by the dominance of planktonic diatom genera and high planktonic/benthicratio (〉40).low lake level and dry climate sustained during 7230~2330 cal.yr BP assuggested by the low abundance of planktonic diatom and low planktonic/benthic ratio ~20and the lake returned to high level during 2330~930 cal.yr BP as inferred by there-dominance of the planktonic diatom and the high value of palnktonic/benthic ratio.The pollen-based climate reconstruction was also consolidated by the grain size andPediastrum concentration records.

Ugii Nuur湖周围现代孢粉研究表明:松属为空气传播的外来花粉,其含量变化可能指示了远山森林草原发育状况;禾本科具显著低代表性,母体植物建群时含量通常在10%以下:藜科花粉含量可以指示区域气候干旱程度。2、以现代孢粉研究为基础、可靠AMS~(14)C年代为框架,Ugii Nuur孢粉记录高分辨率地重建了蒙古国中部地区过去8660 cal.yr BP以来的植被和气候变化。8660~7800 cal.yr BP研究区植被为禾草草原,湖畔及河谷低地发育苔草草甸,远山发育松属针叶林和森林草原,气候温和略湿润;其中8350~8250 cal.yr BP湿生草甸扩张,旱生植物成分减少,气候凉湿。7800~6860 cal.yr BP旱生成分增加,气候转向暖干。6860~3170 cal.yrBP半荒漠草原扩张,远山森林草原退缩,山地草原和河谷及湖畔湿生草甸退缩,气候持续暖干。3170~2340 cal.yr BP半荒漠草原退缩,远山森林草原扩张,气候转凉变湿,末期湿度条件达最佳。2340~1600 cal.yr BP禾草草原发育,湖畔及河谷低地湿生草甸扩张,远山森林草原略有退缩,气候总体较凉湿。1600 cal.yr BP以来研究区发育禾草-冷蒿草原,气候波动较大。

The western Caspian Sea coast is a low-lying and the Turan lowland one, central to the Kazakh hills north of the southern margin of the West Siberian Plain, eastern and southeast are the Altai, tarbagatayn, Huai Gar Alatau and Tien Shan mountain ranges, etc..

西部属里海沿岸低地和图兰低地的一部,中部为哈萨克丘陵,北部为西西伯利亚平原南缘,东部和东南部有阿尔泰、塔尔巴哈台、淮噶尔阿拉套和天山等山脉。

Low German area of East West, the East Low German Low German gradually into the West ...

在东低地德语区的西部,东低地德语逐渐地变为西低地德语。。。。

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