巴西亚马孙流域热带森林的开垦与大豆生产:以朗多尼亚州维列纳市为例

近来巴西大豆生产的增长引发了环境保护团体以及一些学者对于亚马孙盆地的热带自然环境正在向大豆种植地转换的关注.大豆生产的支持者则认为大豆是区域的一种可行性农产品;对于环境的关注是没有根据的,因为新的大豆种植地正在替代已经被砍伐的林地或者是转换了的土地.两种观点虽被提出却都没有对大豆生产扩充区的土地利用与土地覆被(LULC)状况进行过综合研究与估量.本案例研究是在巴西的朗多尼亚州,亚马孙盆地西南部的维列纳市(Vimena),通过遥感手段对1996～2001年以来该市大豆种植面积的大幅度增加所伴随的土地利用与土地覆被变化状况进行评估.结果表明虽然森林变成了大豆生产基地,但是大部分的大豆生产的增长归功于对已有土地的微量扩充、已伐林地的转换以及更高的单位产量.     

Initial Homotypic Cell Pair Adhesion in Regenerating Hydra Facilitates Subsequent Adhesion of Homotypic Cells

 In Hydra vulgaris at the level of dissociated single cells endodermal cells adhere to each other more readily than to ectodermal cells at the initial adhesion. The time required for adhesion to occur between two adjacent cells is shorter for both endodermal and ectodermal homotypic cell adhesions once the initial adhesion of the first pair of cells has been established. It is confirmed that contact of an aggregated pair with additional homotypic cells facilitates the occurrence of homotypic adhesions; heterotypic adhesions are discouraged. This suggests that adhesion of homotypic cells contributes to an increased readiness for subsequent homotypic cells to adhere. Received: 25 August 1999 / Accepted in revised form: 11 January 2000     

Climatic variations in the Eastern Mediterranean Sea area

A very dry climate which prevailed during the last glacial maximum of the Pleistocene from India to the Sahara, was replaced by variable weather conditions with alternating more or less humid phases, starting from the Pleistocene-Holocene transition period and lasting up to about 3000 years ago, when present arid conditions set in. A particularly wet phase is recognized throughout the region some 5000 years ago. Phase shifts within the region and in particular changes in rain distribution patterns, are interpreted as due to shifting spheres of influence of the monsoonal circulation, of Atlantic depressions and moisture originating from the Mediterranean Sea. The condition of the Mediterranean Sea itself, which is influenced by runoff and melt waters from the European Continent and by the Nile floods, as well as by the eustatic sea-level changes, is not a good indicator of local climate conditions.