Publication Date:
2024-02-02
Description:
To understand the role of the ocean within the global carbon cycle, detailed information is required on key-processes within the marine carbon cycle; bio-production in the upper ocean, export of the produced material to the deep ocean and the storage of carbon in oceanic sediments. Quantification of these processes requires the separation of signals of net primary production and the rate of organic matter decay as reflected in fossil sediments. This study examines the large differences in degradation rates of organic-walled dinoflagellate cyst species to separate these degradation and productivity signals. For this, accumulation rates of cyst species known to be resistant (R-cysts) or sensitive (S-cysts) to aerobic degradation of 62 sites are compared to mean annual chlorophyll-a, sea-surface temperature, sea-surface salinity, nitrate and phosphate concentrations of the upper waters and deep-water oxygen concentrations. Furthermore, the degradation of sensitive cysts, as expressed by the degradation constant k and reaction time t, has been related to bottom water [O2]. The studied sediments were taken from the Arabian Sea, north-western African Margin (North Atlantic), western-equatorial Atlantic Ocean/Caraibic, south-western African margin (South Atlantic) and Southern Ocean (Atlantic sector).
Significant relationships are observed between (a) accumulation rates of R-cysts and upper water chlorophyll-a concentrations, (b) accumulation rates of S-cysts and bottom water [O2] and (c) degradation rates of S-cysts (kt) and bottom water [O2].
Relationships that are extremely weak or are clearly insignificant on all confidence intervals are between (1) S-cyst accumulation rates and chlorophyll-a concentrations, sea-surface temperature (SST), sea-surface salinity (SSS), phosphate concentrations (P) and nitrate concentrations (N), (2) between R-cyst accumulation rates and bottom water [O2], SST, SSS, P and N, and between (3) kt and water depth. Co-variance is present between the parameters N and P, N, P and chlorophyll-a, oxygen and water depth. Correcting for this co-variance does not influence the significance of the relationship given above.
The possible applicability of dinoflagellate cyst degradation to estimate past net primary production and deep ocean ventilation is discussed.
Keywords:
906; Accumulation rate, dinoflagellate cysts; Agadir Canyon; Atlantic Caribbean Margin; BC; Box corer; Calculated, see reference(s); Center for Marine Environmental Sciences; Central South Atlantic; Chlorophyll a; DEPTH, sediment/rock; Elevation of event; Event label; GeoB1704-2; GeoB1705-2; GeoB1706-1; GeoB1707-2; GeoB1710-1; GeoB1712-1; GeoB1713-5; GeoB1719-4; GeoB1720-4; GeoB1721-5; GeoB1722-3; GeoB1729-2; GeoB3606-2; GeoB3607-1; GeoB3718-4; GeoB3720-1; GeoB3910-3; GeoB3911-1; GeoB3912-2; GeoB3935-1; GeoB3938-2; GeoB4205-1; GeoB4206-2; GeoB4209-1; GeoB4211-1; GeoB4212-3; GeoB4214-3; GeoB4215-1; GeoB4221-2; GeoB4223-1; GeoB4228-1; GeoB4237-1; GeoB4239-1; GeoB4241-2; GeoB5536-3; GeoB5540-3; GeoB5548-3; GeoB5549-2; GeoB6006-2; GeoB6007-1; GeoB6011-2; GeoB6407-2; GeoB6422-5; GeoB6425-1; GeoB6429-1; Giant box corer; GKG; kt-index; Latitude of event; Longitude of event; M20/2; M34/1; M34/2; M34/4; M37/1; M42/4b; M45/5a; M46/4; MARUM; Meteor (1986); MUC; MultiCorer; Namibia Continental Margin; Namibia continental slope; NIOP-C2; NIOP-C2_902; NIOP-C2_903; NIOP-C2_904; NIOP-C2_905; NIOP-C2_906; NIOP-C2_907; NIOP-C2_908; NIOP-C2_915; NIOP-D2; NIOP-D2_451; NIOP-D2_452; NIOP-D2_453; NIOP-D2_455; NIOP-D2_463; NIOP-D2_464; NIOP-D2_466; Nitrate; Northeast Brasilian Margin; Northern Cape Basin; Oxygen; Phosphate; Sea surface salinity; Sea surface temperature, annual mean; Sea-viewing Wide Field-of-view Sensor (SeaWiFS); Sedimentation rate; see reference(s); Tyro; Walvis Ridge
Type:
Dataset
Format:
text/tab-separated-values, 594 data points
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