Horizontal Distribution and Carbon Biomass of Planktonic Foraminifera in the Eastern Indian Ocean

• Published in: Water
• Main Authors: Sonia Munir, Jun Sun, Steve L. Morton, Xiaodong Zhang, Changling Ding
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2022
• Subjects: planktonic foraminifera; horizontal distribution; diversity; carbon biomass; euphotic zone; Eastern Indian Ocean; Hydraulic engineering; TC1-978; Water supply for domestic and industrial purposes; TD201-500; Indian; Planktonic foraminifera
• Online Access: https://doi.org/10.3390/w14132048; https://doaj.org/article/34f002f8dc6c4338a582d2e2e38fdcd2

Distribution and carbon biomass of planktonic foraminifera were investigated from the euphotic zone of the Eastern Indian Ocean during a two-month cruise, ‘ Shiyan I ’ (10 April–13 May 2014). Foraminifera species were collected through plankton net sampling at 44 locations (80.00°–96.10° E, 10.08° N–6.00° S). The temperature (°C) ranged between 12.82 and 31.8 °C, the salinity ranged between 32.5 and 35.5, and chlorophyll- a concentrations ranged between 0.005 µg/L and 0.89 µg/L. A total of 20 taxa were identified based on the spherical chamber shell, spines, and a final whorl which were examined under light microscopy and scanning electron microscopy. Dominant species that were characterized by the high dominant index Y > 0.14–0.46 were Globigerina bulloides , Globigerinoides ruber white, Globigerinella siphonifera , Turborotalita quinqueloba, and Globigerinella calida , contributing to the community up to 86%. The shell size of collected taxa was from 51 to 508 μm and the total carbon biomass was estimated to be between 0.062 µg C m –3 and 26.52 µg C m –3 . The high carbon biomass was recorded at two stations in the equator zone. Due to its large size, Globorotalia menardii had total carbon biomass of 3.9 µg C m –3 , followed by G. calida 0.68 µg C m −3 , Trilobatus sacculifer 0.38 µg C m –3 , Orbulina universa 0.56 µg C m –3 , and G. ruber white 0.22 µg C m –3 , respectively. The Pearson correlation analysis showed that the temperature and chlorophyll- a were two explanatory environmental variables that were found to be highly significant ( p < 0.05) and that triggered the distribution and abundance of dominant foraminifera species in the study region. Overall, high abundances and carbon biomass were derived from the euphotic zone and equatorial region of the Eastern Indian Ocean.