- 产品描述
Cellabs热带病检验检测试纸
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。
Cellabs热带病检验检测试纸
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。
Cellabs热带病检验检测试纸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】
货号 | 产品名称 | 产品描述 | 规格 | |
免疫荧光试剂盒(IFA kit) | ||||
KR1 | Crypto Cel | 隐孢子虫(Cryptosporidium)间接免疫荧光检测试剂 | 50 Test | |
KR2 | Crypto/Giardia Cel | 隐孢子虫&贾第虫(Cryptosporidium & Giardia)间接免疫荧光检测试剂 | 50 Test | |
KG1 | Giardia Cel | 贾第虫(Giardia)间接免疫荧光检测试剂 | 50 Test | |
KC1 | Chlamydia Cel | 沙眼衣原体(Chlamydia trachomatis)间接免疫荧光检测试剂 | 50 Test | |
KC2 | Chlamydia Cel LPS | 衣原体 lipopolysaccharide (LPS)间接免疫荧光检测试剂 | 50 Test | |
KC3 | Chlamydia Cel Pn | 肺炎衣原体(Chlamydia pneumoniae)间接免疫荧光检测试剂 | 50 Test | |
KP1 | Pneumo Cel | 卡氏肺孢子虫(Pneumocystis carinii)间接免疫荧光检测试剂 | 50 Test | |
KP2 | Pneumo Cel Indirect | 卡氏肺孢子虫( Pneumocystis carinii)间接免疫荧光检测试剂 | 50 Test | |
酶免试剂盒 ELISA kit | ||||
KG2 | Giardia CELISA | 贾第虫(Giardia)ELISA kit | 96 Test | |
KE1 | Entamoeba CELISA Path | 溶组织内阿米巴(Entamoeba histolytica) ELISA kit | 96 Test | |
KF1 & KF2 | Filariasis CELISA | 班氏丝虫(Wuchereria bancrofti ) ELISA kit |
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KM2 | Malaria Antigen (HRP2) CELISA | 恶性疟原虫(Plasmodium falciparum) 抗原 ELISA kit | 192 Test | |
KMC3 | Pan Malaria Antibody CELISA | 间日、三日、恶性及卵形疟疾(Malaria)ELISA IgG kit | 192 Test | |
KT2 | T. cruzi IgG CELISA | 克氏锥虫(Trypanosoma cruzi) ELISA IgG kit | 192 Test | |
KT3 | Toxocara IgG CELISA | 弓首线虫(Toxocara canis) ELISA IgG kit | 192 Test | |
KF3 | Filariasis Ab (Bm14) CELISA | 淋巴丝虫病(lymphatic filariasis) ELISA IgG kit | 480 Test | |
KM7 | Quantimal™ pLDH Malaria CELISA | 疟疾pLDH抗体检测 ELISA kit | 96 Test |
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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】
从以上几个山地垂直自然带分布状况可以知道;山地所处的纬度 愈低,山地海拔高度愈高,山地垂直自然带愈复杂;山地垂直自然带是在山地所处的水平地带基础上形 成和发展起来的,例如乞力马扎罗山位于赤道带,水热条件湿热,所以山麓自然带即基带,属于赤道雨林带(即热带雨林带);长白山处于温带湿润地带,所以基带是温带针叶与落 叶阔叶混交林带。山地地形情况很复杂,例如喜马拉雅山南坡相对高度很大,又处于热带边缘,所以垂直带非常复杂而相当完整;北坡相对高度不大,北坡 坡麓就是青藏高原的一部分,所以垂直自然带比较简单。
海洋自然带指海洋上的自然地理分带。辽 阔的海洋与陆地 相比,其表面非常单一,表层的温度、盐度、水层动态及海洋生物的分布等也都有一定的纬向地带性。 但由于海洋水体具有巨大的流动性,故地带性表现不如大陆明显,各自然带之间的界限只能大体确定, 海洋自然带数目也较少。
海洋自然带的划分,仍以热量带为基础,生物群的分布也是划分海洋自然带的主要标志之一。根据冬季海 洋表层水温的不同,分为冷水(小于0℃)、温水(0°~10℃)、暖水(10°~20℃)和热水(大于20 ℃)等四种类型。结合与海水温度、理化特征和水体运动密切的浮游生物的数量变化,可将世界海 洋分为七个自然带。
(1)北极带。地处高纬区,太阳辐射量较少。冬季干冷,zui冷月1~3月平均温- 30~-40℃;夏季凉爽,7~8月份平均温0~5℃。北极带包括巴伦支海的大部分 水面以外的北冰洋,以及北美东部纽芬兰到冰岛一线西北的大西洋部分。这里表层水温低,又因大陆冰冻期长,江河流入海洋的营 养盐类不多,故海洋生物种数有限,仅在冰融化的边缘海域,才有浮游生物,并将一些鱼类和其它动物 吸引到此处。其中具有经济价值的鱼类主要有北极鳕、白海鲱等;此外,还有鲸目动物(北极鲸或格陵 兰鲸)以及海豹、海象和海鸥、海雀、海鹦等。
(2)北温带。北邻北极带,大体相当于北纬30~60°。全年盛行西风,气候温暖湿润 ,zui热月8月平均温10~22℃,zui冷月2月0~10℃。因受洋流及大气环流影响,大洋东侧的平均温比西侧 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.