Zhang Chuanlun L, Xie Wei, Martin-Cuadrado Ana-Belen, Rodriguez-Valera Francisco
State Key Laboratory of Marine Geology, Tongji University Shanghai, China.
Department of Producción Vegetaly Microbiología, Universidad Miguel Hernández Alicante, Spain.
Front Microbiol. 2015 Oct 13;6:1108. doi: 10.3389/fmicb.2015.01108. eCollection 2015.
Marine Group (MG) I (currently known as Thaumarchaeota) and MG II Archaea were first reported over two decades ago. While significant progress has been made on MG I microbiology and ecology, the progress on MG II has been noticeably slower. The common understanding is that while MG I mainly function as chemolithoautotrophs and occur predominantly in the deep ocean, MG II reside mostly in the photic zone and live heterotrophically. Studies to date have shown that MG II are abundant in the marine aquatic environment and display great seasonal and spatial variation and phylogenetic diversity. They also show unique patterns of organic carbon degradation and their energy requirements may be augmented by light in the photic zone. However, no pure culture of MG II has been obtained and thus their precise ecological role remains elusive.
海洋类群I(目前称为奇古菌门)和海洋类群II古菌早在二十多年前就首次被报道。虽然在海洋类群I的微生物学和生态学方面已经取得了重大进展,但海洋类群II的进展明显较慢。普遍的认识是,海洋类群I主要作为化能无机自养生物发挥作用,主要出现在深海中,而海洋类群II大多栖息在光合带,以异养方式生存。迄今为止的研究表明,海洋类群II在海洋水生环境中数量丰富,表现出很大的季节和空间变化以及系统发育多样性。它们还显示出独特的有机碳降解模式,并且它们的能量需求可能会因光合带中的光照而增加。然而,尚未获得海洋类群II的纯培养物,因此它们的确切生态作用仍然难以捉摸。