We investigated the distribution of nano-sized unicellular Cyanobacteria (nanocyanobacteria) in the Pacific Ocean. Nanocyanobacteria were distributed in the mixed layer throughout the western and central regions of the North and South Pacific subtropical gyres, where nitrate depletion and high irradiance are maintained throughout the year. Their maximum occurrence of >5 × 10 9 cells m -2 was found between 12 and 27°N and 10 and 21°S. These areas with high nanocyanobacterial abundance largely correspond with those with high nitrogen fixation activity. In particular, the biomass of nanocyanobacteria was comparable with or larger than Synechococcus between 10 and 20°N, while in the other regions, Synechococcus was overwhelmingly dominant. Where phosphorus was exhausted at the surface, they were comparatively sparse, even within the western subtropical gyres. In the subtropical and tropical provinces other than the western subtropical gyres, nanocyanobacteria were very sparse, even under similar nutrient conditions where nitrate was depleted and phosphorus was detectable. They may be competing with pico-sized Synechococcus and large filamentous diazotrophic Cyanobacteria Trichodesmium for various resources. Their patchy distribution suggests that the mechanism of nitrogen cycling also varies patchily in the oligotrophic region of the Pacific Ocean.KEY WORDS: Picophytoplankton · Nanophytoplankton · Cyanobacteria · Synechococcus · Pacific subtropical gyres · Cross-basin distribution · Nitrogen fixation
Resale or republication not permitted without written consent of the publisherAquat Microb Ecol 59: [273][274][275][276][277][278][279][280][281][282] 2010 ber & Sarmiento 1997, Deutsch et al. 2001. Additionally, gaseous nitrogen fixation provides the nitrogenlimiting ocean surface with reduced nitrogen, which is available to nondiazotrophs after regeneration by zooplankton or released in the form of dissolved organic compounds (Capone et al. 1994). Traditionally, oceanic nitrogen fixation was considered to be carried out mainly by the filamentous Cyanobacteria of the genus Trichodesmium in the oligotrophic subtropical and tropical waters (Capone et al. 1997). However, after recent observations, nano-sized unicellular Cyanobacteria (nanocyanobacteria) are gaining increasing attention from biogeochemists as important marine nitrogen fixers (Montoya et al. 2004). Molecular biological techniques have revealed that the genes attributable to the nano-sized diazotrophic Cyanobacteria occur extensively in subtropical and tropical waters including the Pacific Ocean (Zehr et al. 2001, Falcón et al. 2004a, Church et al. 2005, Atlantic Ocean (Falcón et al. 2004a, Langlois et al. 2005, Arabian Sea (Mazard et al. 2004) and in Pacific temperate waters (Needoba et al. 2007).While their potential significance in biogeochemical material cycling in the subtropical ocean is well recognized, global distribution of nano-sized Cyanobacteria and their environmental controlling factors are still unknown, since previous observation...