Bacterial response to contrasting geochemistry in the sediments of Central Indian Ocean Basin

The latitudinal differences in geochemical and physiographic nature could evoke varied biological/microbiological response in the deep-sea benthic ecosystem of the Central Indian Ocean. Sediment cores have been examined along latitudinal gradient as a part of the Polymetallic Nodules-Environmental I...

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Bibliographic Details
Main Authors: Anindita Das, Christabelle E. G. Fern, Sonali S. Naik, B. Nagender Nath, Loka Bharathi P. A
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Eia
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.2234
http://drs.nio.org/drs/bitstream/2264/1000/2/Proc_Natl_Semin_PMN_2005_1.pdf
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Summary:The latitudinal differences in geochemical and physiographic nature could evoke varied biological/microbiological response in the deep-sea benthic ecosystem of the Central Indian Ocean. Sediment cores have been examined along latitudinal gradient as a part of the Polymetallic Nodules-Environmental Impact Assessment- Environmental Variability Data Collection (PMN-EIA-EVDC) programme. We present here two such examples of geochemically contrasting cores namely, TVBC-26 and TVBC-08R. Core TVBC-26 (10°S, 75.5°E) is more terrigenously influenced and falls in the siliceous sediment realm and has a relatively higher total organic carbon content (0.37%). Core TVBC-08R (16°S, 75.7°E) falling in the pelagic red clay realm down south is away from the influence of the terrigenous influx and has a lesser total organic carbon value (0.22%). Though the total abundance of bacteria was one order higher in TVBC-08R (1.4x109) as compared to TVBC-26 (7.2x108), the anaerobic viability was one order high in TVBC-26. The viability of bacteria under aerobic condition was marginally high in TVBC-08R. Cells were generally < 1µm in core 08R and ranged from 1.5-1.8µm in core 26. Retrievability of bacteria was in the same order (104.g-1) on different strengths of ZoBell Marine agar suggesting that the bacteria were nutritionally more versatile in core TVBC-08R. Besides, the retrievability of nitrifier was also one order more at this station. 14C uptake at 5°C for 30hrs showed that core TVBC-08R exhibited more autotrophic potential with DPM values of 478+395. g-1 as compared to only 17+ 4. g-1 in core TVBC-26. Thus, under the influence of nutrient starved North Atlantic Deep-Waters [28] the bacterial community at TVBC-08R are nutritionally more flexible as compared to that at TVBC-26, which is bathed by the