Skip to main content
Log in

Bathymetric preference of four major genera of rectilinear benthic foraminifera within oxygen minimum zone in Arabian Sea off central west coast of India

  • Published:
Journal of Earth System Science Aims and scope Submit manuscript

Abstract

Fifty two surface sediment samples collected from the region off Goa, central west coast of India from water depths of 15–3300 m were analyzed with special emphasis on foraminiferal content. Rectilinear benthic foraminiferal morphogroup shows a high relative abundance within Oxygen Minimum Zone (OMZ), both shallow marine (50–60 m water depth) and intermediate to deep water (150–1500 m water depth). We gave special emphasis on four rectilinear foraminiferal genera, namely Fursenkoina, Bolivina, Bulimina and Uvigerina to observe their individual distribution among OMZ. We found genus Fursenkoina predominates at the shallow water OMZ, within the water depth zone of 50–60 m. Within 150–1500 m water depth, which is considered as intermediate to deep water OMZ in this region, genus Uvigerina shows its highest abundance above 1000 m water depth, whereas genus Bulimina shows its affinity with deeper water environment (>1000 m water depth). Genus Bolivina does not show any such depth preference, except its higher abundance in only intermediate to deep water OMZ. This depth differentiation among four rectilinear benthic foraminiferal genera presents the basic data for palaeoclimatic study based on the extent and intensity of OMZ along with the palaeobathymetry study.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Figure 1.
Figure 2.

Similar content being viewed by others

References

  • Alve E 1994 Opportunistic features of the foraminifera Stainforthia fusiformis (Williamson): Evidence from Frierfjord, Norway; J. Micropaleontol. 13 24.

    Article  Google Scholar 

  • Alve E 1995 Benthic foraminiferal distribution and recolonization of formerly anoxic environments in Drammensfjord, southern Norway; Mar. Geol. 25 169–286.

    Google Scholar 

  • Asioli A, Trincardi F, Lowe J J, Ariztegui D, Langone L and Oldfield F 2001 Sub-millennial scale climatic oscillations in the central Adriatic during the Lateglacial: Palaeoceanigraphic implications; Quat. Sci. Rev. 20 1201–1221.

    Article  Google Scholar 

  • Bandy O L 1960 General correlation of foraminiferal structure with environment; In: International Geological Congress, XXI Session (Copenhagen) 22 7–9.

  • Bernhard J M 1992 Benthic foraminiferal distribution and biomass related to porewater oxygen content: Central California continental slope and rise; Deep-Sea Res. 39 585–605.

    Article  Google Scholar 

  • Bernhard J M 1993 Experimental and field evidence of Antarctic foraminiferal tolerance to anoxia and hydrogen sulfide; Mar. Micropal. 20 203–213.

    Article  Google Scholar 

  • Bernhard J M and Sen Gupta B K 1999 Foraminifera of oxygen depleted environments; In: Modern Foraminifera (ed.) Sen Gupta B K, Kluwer Academic Publishers, Dordrecht.

  • Bernhard J M, Sen Gupta B K and Borne P F 1997 Benthic foraminiferal proxy to estimate dysoxic bottom-water oxygen concentrations: Santa Barbara basin, U.S. Pacific continental margin; J. Foram. Res. 27 301–310.

    Article  Google Scholar 

  • Boersma A 1984 Handbook of common Tertiary Uvigerina (New York: Microclimates Press), 207p.

  • Cannariato K G, Kennett J P and Behl R J 1999 Biotic response to Late Quaternary rapid climate switches in Santa Barbara Basin: Ecological and evolutionary implications; Geology 27 63–66.

    Article  Google Scholar 

  • Caralp M H 1987 Deep-sea circulation in the northeastern Atlantic over the past 30,000 years: The benthic foraminiferal record; Oceanol. Acta 10 27–40.

    Google Scholar 

  • Den Dulk M, Reichart G J, Van Heyst S, Zachariasse W J and Van der Zwaan G J 2000 Benthic foraminifera as proxies of organic matter flux and bottom water oxygenation? A case history from the northern Arabian Sea; Palaeogeogr. Palaeoclimatol. Palaeoecol. 161 337–359.

    Article  Google Scholar 

  • Donoso K and Escribano R 2013 Mass-specific respiration of mesozooplankton and its role in the maintenance of an oxygen-deficient ecological barrier (BEDOX) in the upwelling zone off Chile upon presence of a shallow oxygen minimum zone; J. Mar. Sys 129 166–177.

    Article  Google Scholar 

  • Fontanier C, Jorissen F J, Licari L, Alexandre A, Anschutz P and Carbonel P 2002 Live benthic foraminiferal faunas from the Bay of Biscay: Faunal density, composition, and microhabitats; Deep-Sea Res. II 49 751–785.

    Article  Google Scholar 

  • Fuenzalida R, Schneider W, Garces-Vargas J, Bravo L and Lange C 2009 Vertical and horizontal extension of the oxygen minimum zone in the eastern south Pacific Ocean; Deep-Sea Res. II 56 992–1003.

    Article  Google Scholar 

  • Gooday A J 2003 Benthic foraminifera (Protista) as tools in deep-water palaeoceanography: A review of environmental influences on faunal characteristics; Adv. Mar. Biol. 46 1–90.

    Article  Google Scholar 

  • Gooday A J, Bernhard J M, Levin L A and Suhr S B 2000 Foraminifera in the Arabian Sea oxygen minimum zone and other oxygen deficient settings: Taxonomic composition, diversity, and relation to metazoan faunas; Deep-Sea Res. II 47 24–54.

    Google Scholar 

  • Helly J and Levin L A 2004 Global distribution of naturally occurring marine hypoxia on continental margins; Deep-Sea Res. I 51 1159–1168.

    Article  Google Scholar 

  • Hermelin J O R and Shimmield G B 1990 The importance of the oxygen minimum zone and sediment geochemistry in the distribution of Recent benthic foraminifera in the northwest Indian Ocean; Mar. Geol. 91 1–29.

    Article  Google Scholar 

  • Jannink N T, Zachariasse W J and Van der Zwaan G J 1998 Living (Rose Bengal stained) benthic foraminifera from the Pakistan continental margin (North Arabian Sea); Deep-Sea Res. I 45 1483–1513.

    Article  Google Scholar 

  • Jian Z M, Wang L J, Kienast M, Sarnthein M, Kuhnt W, Lin H L and Wang P X 1999 Benthic foraminiferal pale- oceanography of the South China Sea over the last 40,000 years; Mar. Geol. 156 159–186.

    Article  Google Scholar 

  • Jorissen F J 1999 Benthic foraminiferal succession across Late Quaternary Mediterranean sapropels; Mar. Geol. 153 91–101.

    Article  Google Scholar 

  • Jorissen F J, De Stigter H C and Widmark J G V 1995 A conceptual model explaining benthic foraminiferal microhabitats; Mar. Micropal. 26 3–15.

    Article  Google Scholar 

  • Jorissen F J, Wittling I, Peypouquet J P, Rabouille C and Relexans J C 1998 Live benthic foraminiferal faunas off Cape Blance, NW-Africa: Community structure and microhabitates; Deep-Sea Res. I 45 2157– 2188.

    Article  Google Scholar 

  • Kaiho K 1994 Benthic foraminiferal dissolved-oxygen index and dissolved-oxygen levels in the modern ocean; Geology 22 719–722.

    Article  Google Scholar 

  • Kuhnt W, Hess S and Jian Z 1999 Quantitative composition of benthic foraminiferal assemblages as a proxy indicator for organic carbon flux rates in the South China Sea; Mar. Geol. 156 123–127.

    Article  Google Scholar 

  • Levin L A 2003 Oxygen minimum zone benthos: Adaptation and community response to hypoxia; Oceanogr. Mar. Biol. 41 1–45.

    Google Scholar 

  • Levin L A, Gage J D, Martin C and Lamont P A 2000 Macrobenthic community structure within and beneath the oxygen minimum zone, NW Arabian Sea; Deep-Sea Res. II 47 189–226.

    Article  Google Scholar 

  • Lokho K, Venkatachalapathy R and Raju D S N 2004 Uvigerinids and associated foraminifera: Their value as direct evidence for shelf and deep marine paleoenvironments during Upper Disang of Nagaland, Eastern Himalaya and its implications in hydrocarbon exploration; Indian J. Petrol. Geol. 13 79–96.

    Google Scholar 

  • Lutze G F 1986 Uvigerina species of the eastern North Atlantic; Utrecht Micropal. Bull. 35 21–46.

  • Maas M 2000 Verbreitung lebendgefärbter benthischer Foraminiferen in einer intensivierten Sauerstoffminimumzone, Indo-Pakistanischer Kontinentalrand, nördliches Arabisches Meer (Distribution of Rose Bengal stained benthic foraminifera within an intensified oxygen minimum zone, Indo-Pakistan Continental Margin, Northwest Arabian Sea); Meyniana 52 101–128.

    Google Scholar 

  • Mackensen A and Douglas R G 1989 Down-core distribution of live and dead deep-water benthic foraminifera in box cores from the Weddell Sea and the California continental borderland; Deep-Sea Res. 36 879–900.

    Article  Google Scholar 

  • Malakoff D 1998 Death by suffocation in the Gulf of Mexico; Science 281 190–192.

    Article  Google Scholar 

  • Mallon J, Glock N and Schönfeld J 2012 The response of benthic foramonifera to low-oxygen conditions of the Peruvian oxygen minimum zone; In: ANOXIA: Evidence for eukaryote survival and paleontological strategies (eds) Altenbach A V, Bernhard J M and Seckbach J, Cellular Origin, Life in Extreme Habitat and Astrobiology 21 305–321.

  • Mazumder A, Henriques P J and Nigam R 2003 Distribution of benthic foraminifera within oxygen minima zone, off central west coast, India; Gond. Geol. Mag. 6 5–10.

    Google Scholar 

  • Naqvi S W A 1994 Denitrification processes in the Arabian Sea; Proc. Indian Acad. Sci. (Earth Planet. Sci.) 103 279–300.

    Google Scholar 

  • Naqvi S W A, Jayakumar D A, Narvekar P V, Naik H, Sarma V V S S, D’Souza W, Joseph S and George M D 2000 Increased marine production of N 2O due to intensifying anoxia on the Indian continental shelf; Nature 408 346–349.

    Article  Google Scholar 

  • Nigam R, Mazumder A, Henriques P J and Saraswat R 2007 Benthic foraminifera as proxy for oxygen-depleted conditions off the central west coast of India; J. Geol. Soc. India 70 1047–1054.

    Google Scholar 

  • Nigam R, Prasad V, Mazumder A, Garg R, Saraswat R and Henriques P J 2009 Late Holocene changes in hypoxia off the west coast of India: Micropalaeontological evidences; Curr. Sci. 96 708–713.

    Google Scholar 

  • Olson D B, Hitchcock G L, Fine R A and Warren B A 1993 Maintenance of the low-oxygen layer in the central Arabian Sea; Deep-Sea Res. II 40 673–685.

    Article  Google Scholar 

  • Osterman L E 2003 Benthic foraminifers from the continental shelf and slope of the Gulf of Mexico: An indicator of shelf hypoxia; Estuarine Coast. Shelf Sci. 58 17–35.

    Article  Google Scholar 

  • Phleger F B and Soutar A 1973 Production of benthic foraminifera in three east Pacific oxygen minima; Micropaleontol. 19 110–115.

    Article  Google Scholar 

  • Rabalais N N 2000 Oxygen depletion in coastal waters; NOAA State of the Coast Report, National Oceanic and Atmospheric Administration (NOAA), Silver Spring, Maryland; http://state-of-coast.noaa.gov/bulletins/html/hyp_09/hyp.html.

  • Raju D S N and Dave A 1996 Oligocene to Pleistocene uvigerinids and their value in reconstruction of paleodepths in Krishna–Godavari and Cauvery basins; In: Contributions to XV Indian Micropaleontology and Stratigraphy, (eds) Pandey J and Azmi R J et al., Dehra Dun, pp. 189–208.

  • Sarma V V S S 2002 An evaluation of physical and biogeochemical processes regulating the oxygen minimum zone in the water column of the Bay of Bengal; Global Biogeochem. Cycles 16 1099.

    Google Scholar 

  • Schnitker D 1979 Cenozoic deep water foraminifers, Bay of Biscay; In: Init. Repts. DSDP (eds) Montadert L and Roberts D G et al., U.S. Govt. Printing Office, Washington.

  • Schumacher S, Jorissen F J, Dissard D, Larkin K E and Gooday A J 2007 Live (Rose Bengal stained) and dead benthic foraminifera from the oxygen minimum zone of the Pakistan continental margin (Arabian Sea); Mar. Micropal. 62 45–73.

    Article  Google Scholar 

  • Schweizer M, Pawlowski J, Kouwenhoven T J, Guiard J and van der Zwaan B 2008 Molecular phylogeny of Rotaliida (Foraminifera) based on complete small subunit rDNA sequences; Mar. Micropal. 66 233–246.

    Article  Google Scholar 

  • Sen Gupta B K and Machain-Castillo M L 1993 Benthic foraminifera in oxygen-poor habitats; Mar. Micropal. 20 183–201.

    Article  Google Scholar 

  • Sen Gupta R, Braganza A, Noronha R J and Singhbal S Y S 1980 Chemical oceanography of the Arabian Sea. Part V. Hydrochemical characteristics off the central west coast of India; Indian J. Mar. Sci. 9 240–245.

    Google Scholar 

  • Sen Gupta B K, Turner R E and Rabalais N N 1996 Seasonal oxygen depletion in continental-shelf waters of Louisiana: Historical record of benthic foraminifers; Geology 24 227–230.

    Article  Google Scholar 

  • Sen Gupta R, Rajagopal M D and Qasim S Z 1976 Relationship between dissolved oxygen and nutrients in the northwestern Indian Ocean; Indian J. Mar. Sci. 5 201– 211.

    Google Scholar 

  • Sen Gupta R and Naqvi S W A 1984 Chemical oceanography of the Indian Ocean, north of the Equator; Deep-Sea Res. I 31 671–706.

    Article  Google Scholar 

  • Shetye S R, Gouveia A D and Shenoi S S C 1994 Circulation and water masses of the Arabian Sea; In: Biogeochemistry of the Arabian Sea (ed.) Lal D, Proc. Indian Acad. Sci. (Earth Planet. Sci.) 103(2) 107–123.

  • Shibahara A, Ohkushi K, Kennett J P and Ikehara K 2007 Late Quaternary changes in intermediate water oxygenation and oxygen minimum zone, northern Japan: A benthic foraminiferal perspective; Paleoceanogr. 22 PA3213.

    Article  Google Scholar 

  • Spencer R S 1992 Quantified intraspecific variation of common benthic foraminifera from the Northwest Gulf of Mexico: A potential paleobathymetric indicator; J. Foram. Res. 22 274–292.

  • Stackelberg U V 1972 Faziesverteilung in Sedimenten des Indisch-Pakistanischen Kontinental-Randes (Arabisches Meer); Meteor Forschungsgebn Reihe C 9 1–73.

    Google Scholar 

  • Streeter S S and Lavery S A 1982 Holocene and latest glacial benthic foraminifera from the slope and rise off eastern North America; Geol. Soc. Am. Bull. 93 190–199.

    Article  Google Scholar 

  • Streeter S S and Shackleton N J 1979 Paleocirculation of the deep north Atlantic: 150,000 year record of benthic foraminifera and oxygen-18; Science 203 168–171.

    Article  Google Scholar 

  • Swallow J C 1984 Some aspects of the physical oceanography of the Indian Ocean; Deep-Sea Res. 31 639–650.

    Article  Google Scholar 

  • Szarek R, Kuhnt W, Kawamura H and Nishi H 2009 Distribution of recent benthic foraminifera along continental slope of the Sunda Shelf (South China Sea); Mar. Micropal. 71 41–50.

    Article  Google Scholar 

  • Turner R E and Rabalais N N 1994 Coastal eutrophication near the Mississippi river delta; Nature 368 619– 621.

    Article  Google Scholar 

  • Van Leeuwen R J W 1989 Sea-floor distribution and Late Quarternary faunal patterns of planktonic and benthic foraminifers in the Angola basin; Utrecht Micropaleontol. Bull. 38 1–288.

    Google Scholar 

  • Ventura C, Voelker A H L and Fatela F 2010 Benthic foraminifera assemblages as responses to climate variations during MIS 14 to 9 on the mid-depth Portuguese margin; Abstract Volume, Forams 2010, Int. Symp. on Foraminifera, Germany, 194p.

  • Wyrtki K 1962 The oxygen minima in relation to ocean circulation; Deep-Sea Res. Oceanogr. Abstracts 9 11–23.

    Article  Google Scholar 

  • Wyrtki K 1973 Physical oceanography of the Indian Ocean; In: The Biology of the Indian Ocean (ed.) Zeitschel B; Springer, Berlin.

  • You Y and Tomczak M 1993 Thermocline circulation and ventilation in the Indian Ocean derived from water mass analysis; Deep-Sea Res. I 40 13–56.

    Article  Google Scholar 

Download references

Acknowledgements

The authors express their thanks to the Director, Birbal Sahni Institute of Palaeobotany for permission to publish the results. The authors are also thankful to Mrs S M Bhonsle for her help in processing the samples. A M acknowledges the Council of Scientific and Industrial Research, New Delhi for grant.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to ABHIJIT MAZUMDER.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

MAZUMDER, A., NIGAM, R. Bathymetric preference of four major genera of rectilinear benthic foraminifera within oxygen minimum zone in Arabian Sea off central west coast of India. J Earth Syst Sci 123, 633–639 (2014). https://doi.org/10.1007/s12040-014-0419-y

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s12040-014-0419-y

Keywords

Navigation