Living (Rose Bengal stained) benthic foraminiferal faunas along a strong bottom-water oxygen gradient on the Indian margin (Arabian Sea)

Abstract. Rose Bengal stained foraminiferal assemblages were analysed along a five-station bathymetric transect across the core and the lower part of the oxygen minimum zone (OMZ) on the Indian margin of the Arabian Sea. Sediment cores were collected using the manned submersible Shinkai 6500 during RV Yokosuka cruise YK08-11 in the post-monsoon season (October 2008) at water depths ranging from 535 to 2000 m, along a gradient from almost anoxic to well-oxygenated (0.3 to 108 μM) bottom waters. Stained foraminiferal densities were very high in the OMZ core (535 m) and decreased with depth. The faunas were dominated (40–80%) by non-calcareous taxa at all stations. These were mainly species of Reophax and Lagenammina but also included delicate monothalamous taxa (organic-walled "allogromiids", agglutinated saccamminids, psammosphaerids and tubular forms). These new data from the Indian margin are compared to previous studies from the Murray Ridge, the Pakistan margin and the Oman margin. The fact that similar species were found at sites with comparable bottom-water oxygen concentrations but with very different surface water productivity suggests that, within the strongly developed Arabian Sea OMZ, bottom-water oxygen concentration, and not the organic flux to the sea floor, is the main factor controlling the species composition of the foraminiferal communities. Several foraminiferal species (e.g. Praeglobobulimina sp. 1, Ammodiscus sp. 1, Bolivina aff. dilatata) were confined to the core of the OMZ and are presently known only from the Arabian Sea. Because of their association with extremely low-oxygen concentration, these species may prove to be good indicators of past OMZ variability in the Arabian Sea.

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Living (Rose-Bengal-stained) benthic foraminiferal faunas along a strong bottom-water oxygen gradient on the Indian margin (Arabian Sea)

Biogeosciences ◽

10.5194/bg-12-5005-2015 ◽

2015 ◽

Vol 12 (16) ◽

pp. 5005-5019 ◽

Cited By ~ 12

Author(s):

C. Caulle ◽

M. Mojtahid ◽

A. J. Gooday ◽

F. J. Jorissen ◽

H. Kitazato

Keyword(s):

Rose Bengal ◽

Arabian Sea ◽

Bottom Water ◽

Monsoon Season ◽

Water Productivity ◽

Similar Species ◽

Low Oxygen ◽

The Core ◽

Water Oxygen ◽

Oxygen Concentrations

Abstract. Rose-Bengal-stained foraminiferal assemblages (> 150 μm) were analysed along a five-station bathymetric transect across the core and the lower part of the oxygen minimum zone (OMZ) on the Indian margin of the Arabian Sea. Sediment cores were collected using the manned submersible Shinkai 6500 during the RV Yokosuka cruise YK08-11 in the post-monsoon season (October 2008) at water depths ranging from 535 to 2000 m, along a gradient from almost anoxic to well-oxygenated (0.3 to 108 μM) bottom waters. Stained benthic foraminifera were investigated from two different size fractions (150–300 μm and > 300 μm). Stained foraminiferal densities were very high in the core of the OMZ (at 535 and 649 m) and decreased at deeper sites. The faunas (> 150 μm) were dominated (40–80 %) by non-calcareous taxa at all stations. These were mainly species of Reophax and Lagenammina but also included delicate monothalamous taxa (organic-walled "allogromiids", agglutinated saccamminids, psammosphaerids and tubular forms). These new data from the Indian margin are compared to previous studies from the Murray Ridge, the Pakistan margin and the Oman margin. The fact that similar species were found at sites with comparable bottom-water oxygen concentrations but with very different surface water productivity suggests that, within the strongly developed Arabian Sea OMZ, bottom-water oxygen concentration, and not the organic flux to the sea floor, is the main factor controlling the species composition of the foraminiferal communities. Several foraminiferal species (e.g. Praeglobobulimina sp. 1, Ammodiscus sp. 1, Bolivina aff. dilatata) were confined to the core of the OMZ. These species are presently known only from the Arabian Sea. Because of their association with extremely low oxygen concentrations, these species may be good markers for very low oxygen concentrations, and could be used to reconstruct past OMZ variability in the Arabian Sea.

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Live foraminiferal faunas (Rose Bengal stained) from the northern Arabian Sea: links with bottom-water oxygenation

Biogeosciences Discussions ◽

10.5194/bgd-10-15257-2013 ◽

2013 ◽

Vol 10 (9) ◽

pp. 15257-15304 ◽

Cited By ~ 2

Author(s):

C. Caulle ◽

K. A. Koho ◽

M. Mojtahid ◽

G. J. Reichart ◽

F. J. Jorissen

Keyword(s):

Rose Bengal ◽

Arabian Sea ◽

Bottom Water ◽

Principal Component ◽

Environmental Parameters ◽

Low Oxygen ◽

The Core ◽

Northern Arabian Sea ◽

Transitional Group ◽

Epistominella Exigua

Abstract. Live (Rose Bengal stained) benthic foraminifera from the Murray Ridge, within and below the northern Arabian Sea Oxygen Minimum Zone (OMZ), were studied in order to determine the relationship between faunal composition, bottom-water oxygenation (BWO), pore-water chemistry and organic matter (organic carbon and phytopigment) distribution. A series of multicores were recovered from a ten-station oxygen (BWO: 2–78 μM) and bathymetric (885–3010 m depth) transect during the winter monsoon in January 2009. Foraminifera were investigated from three different size fractions (63–125 μm, 125–150 μm and > 150 μm). The larger foraminifera (> 125 μm) were strongly dominated by agglutinated species (e.g. Reophax spp.). In contrast, in the 63–125 μm fraction, calcareous taxa were more abundant, especially in the core of the OMZ, suggesting an opportunistic behaviour. On the basis of a Principal Component Analysis, three foraminiferal groups were identified, reflecting the environmental parameters along the study transect. The faunas from the shallowest stations, in the core of the OMZ (BWO: 2 μM), were composed of "low oxygen" species, typical of the Arabian Sea OMZ (e.g., Rotaliatinopsis semiinvoluta, Praeglobobulimina spp. , Bulimina exilis, Uvigerina peregrina typeparva). These taxa are adapted to the very low BWO conditions and to high phytodetritus supplies. The transitional group, typical for the lower part of the OMZ (BWO: 5–16 μM), is composed of more cosmopolitan taxa tolerant to low-oxygen concentrations (Globocassidulina subglobosa, Ehrenbergina trigona). Below the OMZ (BWO: 26–78 μM), where food availability is more limited and becomes increasingly restricted to surficial sediments, more cosmopolitan calcareous taxa were present, such as Bulimina aculeata, Melonis barleeanus, Uvigerina peregrina and Epistominella exigua. Miliolids were uniquely observed in this last group, reflecting the higher BWO. At these deeper sites, the faunas exhibit a clear depth succession of superficial, intermediate and deep-infaunal microhabitats, because of the deeper oxygen and nitrate penetration into the sediment.

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Live (Rose Bengal stained) foraminiferal faunas from the northern Arabian Sea: faunal succession within and below the OMZ

Biogeosciences ◽

10.5194/bg-11-1155-2014 ◽

2014 ◽

Vol 11 (4) ◽

pp. 1155-1175 ◽

Cited By ~ 36

Author(s):

C. Caulle ◽

K. A. Koho ◽

M. Mojtahid ◽

G. J. Reichart ◽

F. J. Jorissen

Keyword(s):

Rose Bengal ◽

Arabian Sea ◽

Environmental Parameters ◽

Low Oxygen ◽

Organic Input ◽

The Core ◽

Northern Arabian Sea ◽

Transitional Group ◽

Faunal Succession ◽

Epistominella Exigua

Abstract. Live (Rose Bengal stained) benthic foraminifera from the Murray Ridge, within and below the northern Arabian Sea oxygen minimum zone (OMZ), were studied in order to determine the relationship between faunal composition, bottom water oxygenation (BWO), pore water chemistry and organic matter (organic carbon and phytopigment) distribution. A series of multicores were recovered from a ten-station oxygen (BWO: 2–78 μM) and bathymetric (885–3010 m depth) transect during the winter monsoon in January 2009. Foraminifera were investigated from three different size fractions (63–125 μm, 125–150 μm and >150 μm). The larger foraminifera (>125 μm) were strongly dominated by agglutinated species (e.g. Reophax spp.). In contrast, in the 63–125 μm fraction, calcareous taxa were more abundant, especially in the core of the OMZ. On the basis of a principal components analysis, three foraminiferal groups were identified and correlated to the environmental parameters by canonical correspondence analysis. The faunas from the shallowest stations, in the core of the OMZ (BWO: 2 μM), were composed of "low oxygen" species, typical of the Arabian Sea OMZ (e.g. Rotaliatinopsis semiinvoluta, Praeglobobulimina sp., Bulimina exilis, Uvigerina peregrina type parva). These taxa are adapted to the very low BWO conditions and to high phytodetritus supplies. The transitional group, typical for the lower part of the OMZ (BWO: 5–16 μM), is composed of species that are tolerant as well to low-oxygen concentrations, but may be less critical with respect to organic supplies (e.g. Globocassidulina subglobosa, Ehrenbergina trigona). Below the OMZ (BWO: 26–78 μM), where food availability is more limited and becomes increasingly restricted to surficial sediments, cosmopolitan calcareous taxa were present, such as Bulimina aculeata, Melonis barleeanus, Uvigerina peregrina and Epistominella exigua. Miliolids were uniquely observed in this last zone, reflecting the higher BWO and/or lower organic input. At these deeper sites, the faunas exhibit a clear succession of superficial, intermediate and deep infaunal microhabitats, which can be linked to the deeper oxygen and nitrate penetration into the sediment.

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Controlling factors of the OMZ in the Arabian Sea

Biogeosciences Discussions ◽

10.5194/bgd-9-5509-2012 ◽

2012 ◽

Vol 9 (5) ◽

pp. 5509-5550

Author(s):

L. Resplandy ◽

M. Lévy ◽

L. Bopp ◽

V. Echevin ◽

S. Pous ◽

...

Keyword(s):

Spatial Distribution ◽

Oxygen Concentration ◽

Seasonal Cycle ◽

Arabian Sea ◽

Coastal Upwelling ◽

Western Boundary ◽

Ekman Pumping ◽

Low Oxygen ◽

Boundary Current ◽

Ocean Dynamic

Abstract. In-situ observations indicate that the Arabian Sea oxygen minimum zone (OMZ) is only weakly influenced by the strong seasonal cycle of ocean dynamic and biogeochemistry forced by the asian monsoon system and it is spatially decorrelated from the coastal upwelling systems where the biological production is the strongest. In this study we examine the factors controlling the seasonality and the spatial distribution of the OMZ in the Arabian Sea using a coupled bio-physical model. We find that the oxygen concentration in the OMZ displays a seasonal cycle with an amplitude of 5–15 % of the annual mean oxygen concentration. The OMZ is ventilated by lateral ventilation along the western boundary current and in the coastal undercurrent along India during the summer monsoon and by coastal downwelling and negative Ekman pumping during the fall intermonsoon and winter monsoon. This ventilation is counterbalanced by strong coastal upwelling and positive Ekman pumping of low oxygen waters at the base of the OMZ during the spring intermonsoon. Although the factors controlling the OMZ seasonality are associated with the men circulation, we find that mesoscale dynamics modulates them by limiting the vertical ventilation during winter and enhancing it through lateral advection during the rest of the year. Processes explaining the establishment and spatial distribution of the OMZ were quantified using a perturbation experiment initialised with no OMZ. As expected, the oxygen depletion is triggered by strong biological activity in central Arabian Sea during winter and in western and eastern boundary coastal upwelling systems during summer. We find that the 3-D ocean dynamic largely controls the spatial distribution of the OMZ. The eastward shift ensues from the northward lateral transport of ventilated waters along the western and eastern coasts and the advection offshore of low oxygen waters formed in the upwelling system.

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The relationship between pore water carbon isotopic composition and bottom water oxygen concentration

Geochimica et Cosmochimica Acta ◽

10.1016/0016-7037(88)90270-0 ◽

1988 ◽

Vol 52 (5) ◽

pp. 1169-1178 ◽

Cited By ~ 71

Author(s):

Daniel C McCorkle ◽

Steven R Emerson

Keyword(s):

Isotopic Composition ◽

Oxygen Concentration ◽

Pore Water ◽

Bottom Water ◽

Carbon Isotopic Composition ◽

Carbon Isotopic ◽

Water Oxygen ◽

The Relationship

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Benthic oxygen flux, bottom water oxygen concentration and core top organic carbon content in the deep northeast Pacific Ocean

Deep Sea Research Part I Oceanographic Research Papers ◽

10.1016/0967-0637(95)00073-f ◽

1995 ◽

Vol 42 (10) ◽

pp. 1681-1699 ◽

Cited By ~ 43

Author(s):

Wei-Jun Cai ◽

Clare E. Reimers

Keyword(s):

Pacific Ocean ◽

Organic Carbon ◽

Carbon Content ◽

Oxygen Concentration ◽

Bottom Water ◽

Oxygen Flux ◽

Organic Carbon Content ◽

Northeast Pacific ◽

Water Oxygen ◽

Northeast Pacific Ocean

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COMPARISON OF THE IMPROVEMENT EFFECT OF VARIOUS SAND CAPPING MATERIALS ON THE BOTTOM WATER OXYGEN CONCENTRATION

Journal of Japan Society of Civil Engineers Ser B3 (Ocean Engineering) ◽

10.2208/jscejoe.72.i_634 ◽

2016 ◽

Vol 72 (2) ◽

pp. I_634-I_639

Author(s):

Yutaka OKUBO ◽

Koichi YAMADA ◽

Hirokazu TSUJI ◽

Hiromitsu NAGASAKA ◽

Shinsuke HAYAMA ◽

...

Keyword(s):

Oxygen Concentration ◽

Bottom Water ◽

Water Oxygen ◽

Improvement Effect

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Molybdate Corrosion Inhibition in Deaerated and Low-Oxygen Waters

CORROSION ◽

10.5006/1.3583065 ◽

1986 ◽

Vol 42 (9) ◽

pp. 542-545 ◽

Cited By ~ 9

Author(s):

T. R. Weber ◽

M. A. Stranick ◽

M. S. Vukasovich

Keyword(s):

Oxygen Concentration ◽

Sodium Molybdate ◽

Steel Corrosion ◽

Test Methods ◽

Low Oxygen ◽

Electrochemical Test ◽

Synergistic Inhibition ◽

Water Oxygen ◽

Mild Steel Corrosion ◽

Low Oxygen Concentration

Abstract The inhibiting effect of sodium molybdate on mild steel corrosion in deaerated and low-oxygen concentration waters at pH 9.0 and 60 C was investigated using weight loss and electrochemical test methods. Molybdate was inhibitive at a water oxygen concentration between 1 and 2.5 mg/L. In combinations with sodium nitrite, molybdate exhibited synergistic inhibition at 1 mg/L oxygen. An explanation of the observed synergism is discussed based on the electrochemical study.

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