Shell weights of planktonic foraminifera species Globigerinoides ruber in the size range of 300–355 \(\upmu\)m were measured from sediment traps in the western and eastern Arabian Sea which represent upwelling and non-upwelling conditions respectively. In the Western Arabian Sea Trap (WAST), G. ruber flux ranged from 33.3 to 437.3 #/m2/day and shell weights ranged from 6.7 to 14.2 \(\upmu\)g. Whereas, in the Eastern Arabian Sea Trap (EAST), flux ranged from 0.7 to 164.6 #/m2/day and shell weights ranged from 10.4 to 14.8 \(\upmu\)g. Shell weights of G. ruber versus flux showed significant correlation at both the sites which reveals that shell calcification mainly depends on optimal growth conditions. Though the WAST and EAST location have distinct difference in pCO2 and sea surface temperature (SST), the shell weights of G. ruber are similar in these two regions which suggest that surface water pCO2 and SST do not show dominant influence on shell calcification on a seasonal timescale.
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References
Banakar V K, Parthiban G, Patan J N and Jauhari P 1998 Chemistry of surface sediments along a north-south transect across the equator in the central Indian basin: An assessment of biogenic and detrital influences on elemental burial on the seafloor; Chem. Geol. 147 217–232.
Barker S and Elderfield H 2002 Foraminiferal calcification response to glacial–interglacial changes in atmospheric CO2; Sci. 297 833–836.
Bauer S, Hitchcock G L and Olson D B 1991 Influence of monsoonly-forced Ekman dynamics upon surface layer depth and plankton biomass distribution in the Arabian Sea; Deep-Sea Res. A 38 531–553.
Beer C J, Schiebel R and Wilson P A 2010 Testing planktonic foraminiferal shell weight as a surface water [CO\(_{3}^{2-}\)] proxy using plankton net sample; Geol. 38(2) 103–106, doi: 10.1130/G30150.1.
Broecker W S and Clark E 1999 CaCO3 size distribution: A paleocarbonate ion proxy; Paleoceanogr. 14 596–604.
Broecker W S, Clark E, Mc Corkle D C, Peng T-H, Hajdas I and Bonani G 1999 Evidence for a reduction in the carbonate ion content of the deep-sea during the course of the Holocene; Paleoceanogr. 14 744–752.
Broecker W S and Clark E 2001 An evaluation of Lohmann’s foraminifera weight dissolution index; Paleoceanogr. 16(5) 531–534.
Byrne R H, Sabine M, Feely R A and Liu X 2010 Direct observations of basin-wide acidification of the north Pacific Ocean; Geophys. Res. Lett. 37 L02601, doi: 10.1029/2009GL040999.
Conan S M-H, Evanova E M and Brummer G-J A 2002 Quantifying carbonate dissolution and calibration of foraminiferal dissolution indices in the Somali Basin; Mar. Geol. 182 325–349.
Conan S M-H 2006 Calibration of planktic foraminifera proxies for paleoproductivity and seasonal variability in the western Arabian Sea; PhD dissertation, Faculty of Earth and Life Sciences, Vrije Universiteit, Amsterdam, 225p.
Curry W B, Osterman D R, Guptha M V S and Ittekkot V 1992 Foraminiferal production and monsoonal upwelling in the Arabian Sea: Evidence from sediment traps; In: Upwelling Systems; Evolution Since the Early Miocene (eds) Summerhays C P, Prell W L and Emeis K C; Geol. Soc. of London, England, pp. 93–106.
de Moel H, Ganssen G M, Peeters F J C, Jung S J A, Kroon D, Brummer G J A and Zeebe R E 2009 Planktic foraminiferal shell thinning in the Arabian Sea due to anthropogenic ocean acidification?; Biogeosci. 6 1917–1925.
de Villiers S 2004 Occupation of an ecological niche as the fundamental control on the shell-weight of calcifying planktonic foraminifera; Mar. Biol. 144(1) 45–50.
Hemleben C and Spindler M 1983 Recent advances in research on living planktonic foraminifera; Utrecht Micropal. Bull. 30 141–170.
Honjo W and Doherty K W 1988 Large aperture time series oceanic sediment traps: Design objectives, construction and application; Deep-Sea Res. 35 133–149.
Honjo S, Manganini S, Krishfield R A and Francois R 2008 Particulate organic carbon fluxes to the ocean interior and factors controlling the biological pump: A synthesis of global sediment trap programs since 1983; Progr. Oceanogr. 76 217–285.
Lendt R, Thomas H, Hupe A and Ittekkot V 2003 Response of the near-surface carbonate system of the northwestern Arabian Sea to the southwest monsoon and related biological forcing; J. Geophys. Res. 108 3222, doi: 10.1029/2000JC000771.
Lohmann G P 1995 A model for variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolution; Paleoceanogr. 10 445–447.
Madhupratap M, Kumar S P, Bhattathiri P M A, Kumar M D, Raghukumar S, Nair K K C and Ramaiah N 1996 Mechanism of the biological response to winter cooling in the Arabian Sea; Nature 384 549–551.
Mohan R, Verma K, Mergulhao L P, Sinha D K, Shanavas S and Guptha M V S 2006 Seasonal variations of pteropods from the Western Arabian Sea sediment traps; Geo-Mar. Lett. 26 265–273.
Naik S S, Naidu P D, Govil P and Godad S 2010 Relationship between weights of planktonic foraminifer shell and surface water CO\(_{3}^{=}\) concentration during the Holocene and Last Glacial Period; Mar. Geol. 275 278–282.
Peeters F J C, Brummer G-J A and Ganssen G 2002 The effect of upwelling on the distribution and stable isotope composition of Globigerina bulloides and Globigerinoides ruber (planktic foraminifera) in modern surface waters of the NW Arabian Sea; Glob. Planet. Change 34(3–4) 269–291.
Qasim S Z 1982 Oceanography of the northern Arabian Sea; Deep-Sea Res. A 29 1041–1068.
Schiebel R, Zeltner A, Treppke U F, Waniek J J, Bollmann J, Rixen T and Hemleben C 2004 Distribution of diatoms, coccolithophores and planktic foraminifers along atrophic gradient during SW monsoon in the Arabian Sea; Mar. Micropal. 51 345–371, doi: 10.1016/j.marmicro.2004.02.001.
Schmidt D N, Lazarus D, Young J R and Kucera M 2006 Biogeography and evolution of body size in marine plankton; Earth-Sci. Rev. 78 239–266.
Schott F 1983 Monsoon response of the Somalia Current and associated upwelling; Progr. Oceanogr. 12(3) 357–381.
Shallow J C 1984 Some aspects of the physical oceanography of the Indian Ocean; Deep-Sea Res. A 31 639–650.
Takahashi T, Sutherland S C and Wanninkhof R et al. 2009 Climatological mean and decadal changes in surface ocean pCO2, and net sea–air CO2 flux over the global oceans; Deep-Sea Res. II 56 554–577.
Wang W 2000 Isotopic signals in two morphotypes of Globigerinoides ruber (white) from the South China Sea: Implications for monsoon climate change during the last glacial cycle; Paleogeogr. Paleoclimatol. Paleoecol. 161 381–394.
Wyrtki K 1973 Physical oceanography of the Indian Ocean; In: The Biology of the Indian Ocean (ed.) Zeitzschelp B (New York: Springer-Verlag), pp. 18–36.
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The authors thank Dr S Shetye, Director, National Institute of Oceanography for support and encouragement. This is NIO Contribution No. 5315.
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NAIK, S.S., GODAD, S.P., NAIDU, P.D. et al. A comparison of Globigerinoides ruber calcification between upwelling and non-upwelling regions in the Arabian Sea. J Earth Syst Sci 122, 1153–1159 (2013). https://doi.org/10.1007/s12040-013-0330-y
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DOI: https://doi.org/10.1007/s12040-013-0330-y