创仑检验检测热带病测试纸

广州健仑生物科技有限公司

广州健仑长期供应各种生物原料，主要代理品牌：美国Seracare、西班牙Certest、美国Fuller、美国NOVABIOS、 Cellabs等等。

Cellabs公司是一个的生物技术公司，总部位于澳大利亚悉尼。专门研发与生产针对热带传染性疾病的免疫诊断试剂盒。其产品40多个国家和地区。1998年，Cellabs收购TropBio公司，进一步巩固其在研制热带传染病、寄生虫诊断试剂方面的位置。

创仑检验检测热带病测试纸
    该公司的Crypto/Giardia Cel IFA是国标*推荐的两虫检测IFA染色试剂、Crypto Cel Antibody Reagent是UK DWI水质安全评估检测的*抗体。

主要产品包括：隐孢子虫诊断试剂，贾第虫诊断试剂，疟疾诊断试剂，衣原体检测试剂，丝虫诊断试剂，锥虫诊断试剂等。

广州健仑生物科技有限公司与cellabs达成代理协议，欢迎广大用户咨询订购。

我司还提供其它进口或国产试剂盒：登革热、疟疾、流感、A链球菌、合胞病毒、腮病毒、乙脑、寨卡、黄热病、基孔肯雅热、克锥虫病、违禁品滥用、肺炎球菌、军团菌、化妆品检测、食品安全检测等试剂盒以及日本生研细菌分型诊断血清、德国SiFin诊断血清、丹麦SSI诊断血清等产品。

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【Seracare产品介绍】

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【公司名称】 广州健仑生物科技有限公司
【】    杨永汉 
【】 
【腾讯 】 2042552662
【公司地址】 广州清华科技园创新基地番禺石楼镇创启路63号二期2幢101-3室
【企业文化】

南温带气候类型主要包括温带海洋性气候和温带大陆性气候两种
温带海洋性气候主要分布在南、北纬40°～60°的大陆西岸，南温带的温带海洋性气候主要分布在南美洲南部的西海岸，大洋洲的南部地区。这里终年受来自海洋的西风带的影响，所以全年温和湿润，降水季节分配比较均匀。植被类型主要为温带落叶阔叶林。
温带大陆性气候主要分布在南美洲南部的东部地区。南温带的温带大陆性气候成因和北温带的温带大陆性气候类型的成因不同。南半球没有像亚欧大陆那样宽广的大陆，所以其降水稀少的温带大陆性气候不是因距海远造成的，一般是由于处于高大山脉的背风坡造成的。如南美南端的温带大陆性气候是在西风带的影响下，处于安第斯山的背风坡，所以降水稀少，形成温带草原和荒漠景观。
南温带的海洋生物的生长和发育条件与北温带相似。海洋内植物生长繁茂，巨型藻类多，浮游生物也很丰富。南温带在南半球是海洋动物zui多的地带，那里生活着南、北温带都可见到的动物类型，如海狗、海豹、鲸，还有刀鱼、鰯鱼、小鳁鱼、鲨鱼等。每逢冬季，有来自南方的海洋动物到此越冬，当夏季时，又有热带海洋动物前来肥育。受离岸风的影响，在非洲大陆西南部和南美洲的秘鲁沿海有上升流存在，因此深层海水中的有机物质和营养盐类随着上升流来到海水表层，这使此地浮游生物大量繁殖，为鱼类提供了丰富的饵料，因而鱼类在此积聚，形成南半球重要的捕捞区。
大陆水平自然带是纬度地带性和经度地带性两种规律共同作用的结果。在前者占优势的地区，自然带沿纬线方向伸展；后者 占优势的地区，自然带沿经线方向伸展；两者作用相近的地区，自然带与经纬线交叉。山地垂直自然带的分布随高度而变化。
自然带[1]  的形成主要与地球表面的太阳辐射能在各纬度分布不均有关，在各大陆和大洋都形成一系列自然带。由于大陆自然带的形成不仅受纬度热力分带的影响，而且受到海陆分布、地势起伏的干扰，所以大陆自然带比大洋表层的自然带复杂得多。
The temperate climate in South China mainly includes temperate maritime climate and temperate continental climate.
The temperate maritime climate is mainly distributed on the west coast of the mainland with latitudes of 40° to 60° North and South. The temperate maritime climate in the South Temperate Zone is mainly distributed on the west coast of southern South America and the southern part of Oceania. It is affected by the westerly winds from the ocean all year round, so it is mild and humid throughout the year and the precipitation season is evenly distributed. The vegetation type is mainly temperate deciduous broad-leaved forest.
The temperate continental climate is mainly distributed in the eastern part of southern South America. The temperate continental climate in the southern temperate and the temperate continental climate in the north temperate have different causes. The southern hemisphere does not have a continent as wide as the Eurasian continent. Therefore, the temperate continental climate with few precipitation is not caused by the distance from the sea. It is usually caused by the leeward slope of the high mountains. For example, the temperate continental climate at the southern tip of South America is under the influence of the westerly belt and is located on the leeward slope of the Andean Mountains, so the precipitation is scarce, forming temperate grasslands and desert landscapes.
The temperate marine growth and development conditions in the South Temperate Zone are similar to those in the north temperate zone. The plants in the sea grow abundantly, with many giant algae and abundant plankton. The southern temperate zone is the most marine animal in the southern hemisphere. It is home to the types of animals found in the temperate regions of the south and north, such as seals, seals and whale, as well as saury, squid, small squid, and sharks. In winter, there are marine animals from the south to winter, and in the summer, tropical sea animals come to fatten. Affected by offshore winds, there are upwellings on the Peruvian coast in the southwestern part of the African continent and South America. As a result, organic matter and nutrients in the deep seawater come up to the surface of the sea with rising water, which causes the plankton to multiply in this area. It provides abundant fish for the fish, so the fish accumulate here, forming an important fishing area in the southern hemisphere.
The horizontal natural zone of the continent is the result of the joint action of latitudinal zonality and longitude zonality. In areas where the former are predominant, natural belts stretch in the direction of the latitude line; in the latter-dominated areas, natural belts stretch in the direction of meridians; in areas where the two are similar, natural belts intersect with latitude and longitude lines. The distribution of vertical natural belts varies with height.
The formation of the natural belt [1] is mainly related to the uneven distribution of solar radiation at various latitudes on the surface of the Earth. A series of natural belts are formed in each continent and ocean. Because the formation of the natural belt in the mainland is not only affected by latitudinal thermal zoning, but also by land and sea distribution and undulating terrain, the natural belt of the mainland is much more complex than the natural belt of the oceanic surface.