- 產品描述
Cellabs熱帶病檢驗檢測試紙
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。
Cellabs熱帶病檢驗檢測試紙
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。
Cellabs熱帶病檢驗檢測試紙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】
貨號 | 產品名稱 | 產品描述 | 規格 | |
免疫熒光試劑盒(IFA kit) | ||||
KR1 | Crypto Cel | 隱孢子蟲(Cryptosporidium)間接免疫熒光檢測試劑 | 50 Test | |
KR2 | Crypto/Giardia Cel | 隱孢子蟲&賈第蟲(Cryptosporidium & Giardia)間接免疫熒光檢測試劑 | 50 Test | |
KG1 | Giardia Cel | 賈第蟲(Giardia)間接免疫熒光檢測試劑 | 50 Test | |
KC1 | Chlamydia Cel | 沙眼衣原體(Chlamydia trachomatis)間接免疫熒光檢測試劑 | 50 Test | |
KC2 | Chlamydia Cel LPS | 衣原體 lipopolysaccharide (LPS)間接免疫熒光檢測試劑 | 50 Test | |
KC3 | Chlamydia Cel Pn | 肺炎衣原體(Chlamydia pneumoniae)間接免疫熒光檢測試劑 | 50 Test | |
KP1 | Pneumo Cel | 卡氏肺孢子蟲(Pneumocystis carinii)間接免疫熒光檢測試劑 | 50 Test | |
KP2 | Pneumo Cel Indirect | 卡氏肺孢子蟲( Pneumocystis carinii)間接免疫熒光檢測試劑 | 50 Test | |
酶免試劑盒 ELISA kit | ||||
KG2 | Giardia CELISA | 賈第蟲(Giardia)ELISA kit | 96 Test | |
KE1 | Entamoeba CELISA Path | 溶組織內阿米巴(Entamoeba histolytica) ELISA kit | 96 Test | |
KF1 & KF2 | Filariasis CELISA | 班氏絲蟲(Wuchereria bancrofti ) ELISA kit |
| |
KM2 | Malaria Antigen (HRP2) CELISA | 惡性瘧原蟲(Plasmodium falciparum) 抗原 ELISA kit | 192 Test | |
KMC3 | Pan Malaria Antibody CELISA | 間日、三日、惡性及卵形瘧疾(Malaria)ELISA IgG kit | 192 Test | |
KT2 | T. cruzi IgG CELISA | 克氏錐蟲(Trypanosoma cruzi) ELISA IgG kit | 192 Test | |
KT3 | Toxocara IgG CELISA | 弓首線蟲(Toxocara canis) ELISA IgG kit | 192 Test | |
KF3 | Filariasis Ab (Bm14) CELISA | 淋巴絲蟲病(lymphatic filariasis) ELISA IgG kit | 480 Test | |
KM7 | Quantimal™ pLDH Malaria CELISA | 瘧疾pLDH抗體檢測 ELISA kit | 96 Test |
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】
從以上幾個山地垂直自然帶分布狀況可以知道;山地所處的緯度 愈低,山地海拔高度愈高,山地垂直自然帶愈復雜;山地垂直自然帶是在山地所處的水平地帶基礎上形 成和發展起來的,例如乞力馬扎羅山位于赤道帶,水熱條件濕熱,所以山麓自然帶即基帶,屬于赤道雨林帶(即熱帶雨林帶);長白山處于溫帶濕潤地帶,所以基帶是溫帶針葉與落 葉闊葉混交林帶。山地地形情況很復雜,例如喜馬拉雅山南坡相對高度很大,又處于熱帶邊緣,所以垂直帶非常復雜而相當完整;北坡相對高度不大,北坡 坡麓就是青藏高原的一部分,所以垂直自然帶比較簡單。
海洋自然帶指海洋上的自然地理分帶。遼 闊的海洋與陸地 相比,其表面非常單一,表層的溫度、鹽度、水層動態及海洋生物的分布等也都有一定的緯向地帶性。 但由于海洋水體具有巨大的流動性,故地帶性表現不如大陸明顯,各自然帶之間的界限只能大體確定, 海洋自然帶數目也較少。
海洋自然帶的劃分,仍以熱量帶為基礎,生物群的分布也是劃分海洋自然帶的主要標志之一。根據冬季海 洋表層水溫的不同,分為冷水(小于0℃)、溫水(0°~10℃)、暖水(10°~20℃)和熱水(大于20 ℃)等四種類型。結合與海水溫度、理化特征和水體運動密切的浮游生物的數量變化,可將世界海 洋分為七個自然帶。
(1)北極帶。地處高緯區,太陽輻射量較少。冬季干冷,zui冷月1~3月平均溫- 30~-40℃;夏季涼爽,7~8月份平均溫0~5℃。北極帶包括巴倫支海的大部分 水面以外的北冰洋,以及北美東部紐芬蘭到冰島一線西北的大西洋部分。這里表層水溫低,又因大陸冰凍期長,江河流入海洋的營 養鹽類不多,故海洋生物種數有限,僅在冰融化的邊緣海域,才有浮游生物,并將一些魚類和其它動物 吸引到此處。其中具有經濟價值的魚類主要有北極鱈、白海鯡等;此外,還有鯨目動物(北極鯨或格陵 蘭鯨)以及海豹、海象和海鷗、海雀、海鸚等。
(2)北溫帶。北鄰北極帶,大體相當于北緯30~60°。全年盛行西風,氣候溫暖濕潤 ,zui熱月8月平均溫10~22℃,zui冷月2月0~10℃。因受洋流及大氣環流影響,大洋東側的平均溫比西側 低5℃。
It can be known from the distribution of the above-mentioned vertical natural belts; the lower the latitude of the mountainous area, the higher the altitude of the mountain, and the more complex the vertical natural belt of the mountain; the vertical natural belt of the mountain is formed on the basis of the horizontal zone where the mountain is located and Developed, for example, Mount Kilimanjaro is located in the equatorial belt, hot and humid conditions, so the natural belt is the base belt, belongs to the equatorial rainforest belt (ie, tropical rain forest belt); Changbai Mountain is in the temperate humid zone, so the base belt is temperate needles and Deciduous broad-leaved mixed forest zone. The terrain of the mountainous terrain is very complex. For example, the southern slope of the Himalayas is relatively high in height and on the edge of the tropics, so the vertical belt is very complex and quite complete; the northern slope is relatively small, and the northern slope is part of the Tibetan Plateau, so the vertical natural belt easier.
The natural zone of the ocean refers to the natural geographical division on the ocean. Compared with land, the vast ocean has a very simple surface. The surface temperature, salinity, dynamics of the water layer, and the distribution of marine organisms also have certain zonal zonality. However, due to the huge fluidity of oceanic water bodies, the zonal performance is not as pronounced as that of the mainland. The boundary between natural belts can only be roughly determined, and the number of marine natural belts is also small.
The division of the natural belts of the sea is still based on heat bands, and the distribution of biota is also one of the main signs that divide the natural belts of the oceans. According to the difference of surface water temperature in winter, it can be divided into four types: cold water (less than 0°C), warm water (0°~10°C), warm water (10°~20°C) and hot water (greater than 20°C). Combined with changes in the number of plankton that are closely linked to seawater temperature, physical and chemical characteristics, and water movement, the world's oceans and oceans can be divided into seven natural zones.
(1) Arctic belt. Located in high latitudes, there is less solar radiation. Dry and cold in winter, the coldest month average temperature from January to March - 30 ~ -40 °C; summer cool, 7 ~ August average temperature 0 ~ 5 °C. The Arctic belt includes most of the Arctic Ocean outside the Barents Sea, and Newfoundland in North America and Iceland in the northwestern part of the line. The surface water temperature here is low, and because of the long frozen period in the mainland, there are not many types of nutrients in rivers and seas, so the number of marine species is limited. Plankton are found only in the frigid seas where ice melts, and some fish and other animals are found. Attracted here. Among the fish that have economic value are Arctic eel and white sea bream. In addition, there are also cetaceans (Arctic whales or Green whale) and seals, walruses and gulls, puffins, puffins and so on.
(2) North Temperate Zone. North of the North Pole, roughly equivalent to 30 to 60 degrees north latitude. The prevailing westerly winds throughout the year have a warm and humid climate. The average temperature of the hottest month of August is 10 to 22°C, and that of the coldest month is 0 to 10°C. Due to ocean currents and atmospheric circulation, the average temperature on the east side of the ocean is 5°C lower than on the west side.