AN EXTENSIVE BLOOM OF THE N-2-FIXING CYANOBACTERIUM TRICHODESMIUM-ERYTHRAEUM IN THE CENTRAL ARABIAN SEA

Citation
Dg. Capone et al., AN EXTENSIVE BLOOM OF THE N-2-FIXING CYANOBACTERIUM TRICHODESMIUM-ERYTHRAEUM IN THE CENTRAL ARABIAN SEA, Marine ecology. Progress series, 172, 1998, pp. 281-292
Citations number
44
Categorie Soggetti
Marine & Freshwater Biology",Ecology
ISSN journal
01718630
Volume
172
Year of publication
1998
Pages
281 - 292
Database
ISI
SICI code
0171-8630(1998)172:<281:AEBOTN>2.0.ZU;2-7
Abstract
We encountered an extensive surface bloom of the N-2 fixing cyanobacte rium Trichodesmium erythraeum in the central basin of the Arabian Sea during the spring inter-monsoon of 1995. The bloom, which occurred dur ing a period of calm winds and relatively high atmospheric iron conten t, was metabolically active. Carbon fixation by the bloom represented about one-quarter of water column primary productivity while input by N-2 fixation could account for a major fraction of the estimated 'new' N demand of primary production. Isotopic measurements of the N in sur face suspended material confirmed a direct contribution of N-2 fixatio n to the organic nitrogen pools of the upper water column. Retrospecti ve analysis of NOAA-12 AVHRR imagery indicated that blooms covered up to 2 x 10(6) km(2), or 20% of the Arabian Sea surface, during the peri od from 22 to 27 May 1995. In addition to their biogeochemical impact, surface blooms of this extent may have secondary effects on sea surfa ce albedo and light penetration as well as heat and gas exchange acros s the air-sea interface. A preliminary extrapolation based on our obse rved, non-bloom rates of N-2 fixation from our limited sampling in the spring intermonsoon, including a conservative estimate of the input b y blooms, suggest N-2 fixation may account for an input of about 1 Tg N yr(-1). This is substantial, but relatively minor compared to curren t estimates of the removal of N through denitrification in the basin. However, N-2 fixation may also occur in the central basin through the mild winter monsoon, be considerably greater during the fall intermons oon than we observed during the spring intermonsoon, and may also occu r at higher levels in the chronically oligotrophic southern basin. Ong oing satellite observations will help to determine more accurately the distribution and density of Trichodesmium in this and other tropical oceanic basins, as well as resolving the actual frequency and duration of bloom occurrence.