創侖檢驗檢測熱帶病測試紙

廣州健侖生物科技有限公司

廣州健侖長期供應各種生物原料，主要代理品牌：美國Seracare、西班牙Certest、美國Fuller、美國NOVABIOS、 Cellabs等等。

Cellabs公司是一個的生物技術公司，總部位于澳大利亞悉尼。專門研發與生產針對熱帶傳染性疾病的免疫診斷試劑盒。其產品40多個國家和地區。1998年，Cellabs收購TropBio公司，進一步鞏固其在研制熱帶傳染病、寄生蟲診斷試劑方面的位置。

創侖檢驗檢測熱帶病測試紙
    該公司的Crypto/Giardia Cel IFA是國標*推薦的兩蟲檢測IFA染色試劑、Crypto Cel Antibody Reagent是UK DWI水質安全評估檢測的*抗體。

主要產品包括：隱孢子蟲診斷試劑，賈第蟲診斷試劑，瘧疾診斷試劑，衣原體檢測試劑，絲蟲診斷試劑，錐蟲診斷試劑等。

廣州健侖生物科技有限公司與cellabs達成代理協議，歡迎廣大用戶咨詢訂購。

我司還提供其它進口或國產試劑盒：登革熱、瘧疾、流感、A鏈球菌、合胞病毒、腮病毒、乙腦、寨卡、黃熱病、基孔肯雅熱、克錐蟲病、違禁品濫用、肺炎球菌、軍團菌、化妝品檢測、食品安全檢測等試劑盒以及日本生研細菌分型診斷血清、德國SiFin診斷血清、丹麥SSI診斷血清等產品。

歡迎咨詢

歡迎咨詢2042552662

【Seracare產品介紹】

二維碼掃一掃

【公司名稱】 廣州健侖生物科技有限公司
【】    楊永漢 
【】 
【騰訊 】 2042552662
【公司地址】 廣州清華科技園創新基地番禺石樓鎮創啟路63號二期2幢101-3室
【企業文化】

南溫帶氣候類型主要包括溫帶海洋性氣候和溫帶大陸性氣候兩種
溫帶海洋性氣候主要分布在南、北緯40°～60°的大陸西岸，南溫帶的溫帶海洋性氣候主要分布在南美洲南部的西海岸，大洋洲的南部地區。這里終年受來自海洋的西風帶的影響，所以全年溫和濕潤，降水季節分配比較均勻。植被類型主要為溫帶落葉闊葉林。
溫帶大陸性氣候主要分布在南美洲南部的東部地區。南溫帶的溫帶大陸性氣候成因和北溫帶的溫帶大陸性氣候類型的成因不同。南半球沒有像亞歐大陸那樣寬廣的大陸，所以其降水稀少的溫帶大陸性氣候不是因距海遠造成的，一般是由于處于高大山脈的背風坡造成的。如南美南端的溫帶大陸性氣候是在西風帶的影響下，處于安第斯山的背風坡，所以降水稀少，形成溫帶草原和荒漠景觀。
南溫帶的海洋生物的生長和發育條件與北溫帶相似。海洋內植物生長繁茂，巨型藻類多，浮游生物也很豐富。南溫帶在南半球是海洋動物zui多的地帶，那里生活著南、北溫帶都可見到的動物類型，如海狗、海豹、鯨，還有刀魚、鰯魚、小鳁魚、鯊魚等。每逢冬季，有來自南方的海洋動物到此越冬，當夏季時，又有熱帶海洋動物前來肥育。受離岸風的影響，在非洲大陸西南部和南美洲的秘魯沿海有上升流存在，因此深層海水中的有機物質和營養鹽類隨著上升流來到海水表層，這使此地浮游生物大量繁殖，為魚類提供了豐富的餌料，因而魚類在此積聚，形成南半球重要的捕撈區。
大陸水平自然帶是緯度地帶性和經度地帶性兩種規律共同作用的結果。在前者占優勢的地區，自然帶沿緯線方向伸展；后者 占優勢的地區，自然帶沿經線方向伸展；兩者作用相近的地區，自然帶與經緯線交叉。山地垂直自然帶的分布隨高度而變化。
自然帶[1]  的形成主要與地球表面的太陽輻射能在各緯度分布不均有關，在各大陸和大洋都形成一系列自然帶。由于大陸自然帶的形成不僅受緯度熱力分帶的影響，而且受到海陸分布、地勢起伏的干擾，所以大陸自然帶比大洋表層的自然帶復雜得多。
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.