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Veeran, Yoganandan (2023): Organic carbon, calcium carbonate contents, mass accumulation rate, burial efficiency, and paleoproductivity record from a sediment core SK-313 GC01 southeastern Arabian Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.946959

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Abstract:
Variations in the paleoproductivity during the last 14.4 kyr have been studied using organic carbon (OC), calcium carbonate (CaCO3) contents and their mass accumulation rate and burial efficiency, in a 14C-dated sediment core (SK 313 GC-01; 4.82-m) from the southeastern Arabian Sea. The core was sub-sampled at 1-cm intervals for the top 1 m and 2-cm intervals for the rest of the core. All subsamples were oven-dried at 40°C and finely powdered in an agate mortar with a pestle. CaCO3 content was determined by Ethylene Diamine Tetra-Acetic acid (EDTA) titration using Patton & Reader as an indicator (Shapiro and Brannock, 1962, doi:10.3133/b1144A). The OC content was determined by chromic acid digestion and subsequent titration with ferrous ammonium sulfate as described in Gaudette et al. (1974, doi:10.1306/74D729D7-2B21-11D7-8648000102C1865D). We note that paleoproductivity was the highest during the Bølling–Allerød warm event; a step-wise decreased productivity during the Younger Dryas cold period, the lowest productivity during the early Holocene, and increased and stabilized productivity during the mid-late Holocene interval.
Keyword(s):
Calcium Carbonate; marine sediments; Organic carbon; paleoproductivity; southeastern Arabian Sea
Related to:
Veeran, Yoganandan (submitted): A 14.4 kyr record of paleoproductivity changes in the southeastern Arabian Sea. Marine Geology
Funding:
Department of Science and Technology (DST), grant/award no. 496/2014
Coverage:
Latitude: 10.501800 * Longitude: 75.375000
Date/Time Start: 2014-06-08T15:49:11 * Date/Time End: 2014-06-08T15:49:11
Minimum Elevation: -513.2 m * Maximum Elevation: -513.2 m
Event(s):
SK313_GC-01 * Latitude: 10.501800 * Longitude: 75.375000 * Date/Time: 2014-06-08T15:49:11 * Elevation: -513.2 m * Location: North Indian Ocean/ Southeastern Arabian Sea * Method/Device: Core (CORE)
Comment:
Accumulation rate (MAR) of OC and CaCO3 (g/m²/a) was calculated using the following formula: OC (CaCO3) = (OC (CaCO3)×DBD×LSR)/100.
Paleoproductivity (g/cm²/a) was estimated using the following formula by Stein (1986, hdl:10013/epic.14450): Paleoproductivity (PP) = 5.31 [OC (DBD)]0.71× LSR0.07 × WD0.45.
Burial efficiency (BE, %) of OC was estimated using the following formula by Bhushan et al. (2001, doi:10.1016/S0025-3227(01)00179-7): BE (%) = [(Burial Flux)/Productivity]×100.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1AGEAgeka BPVeeran, YoganandanGeocode
2Carbon, organicC org%Veeran, YoganandanSee description in dataset commentwt. %
3Calcium carbonateCaCO3%Veeran, YoganandanSee description in dataset commentwt. %
4Accumulation rate, carbon, organicAcc rate C orgg/cm2/aVeeran, YoganandanSee description in dataset comment
5Accumulation rate, calcium carbonateAcc rate CaCO3g/cm2/aVeeran, YoganandanSee description in dataset comment
6Burial rate of organic carbonOC burg/cm2/aVeeran, YoganandanSee description in dataset comment
7Burial rate of calcium carbonateCaCO3 burg/cm2/aVeeran, YoganandanSee description in dataset comment
8Burial efficiency of calcium carbonateCaCO3 bur eff%Veeran, YoganandanDetermined according to Bhushan et al. (2001)
9Paleoproductivity, as organic carbonPP OCg/cm2/aVeeran, YoganandanPP calculated (Stein, 1986)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
1928 data points

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