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Conte, Maureen H; Eginton, G (1993): (Table 2) Distribution of alkenone unsaturation index UK37 of the eastern North Atlantic [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.67009, Supplement to: Conte, Maureen H; Eglinton, Geoffrey (1993): Alkenone and alkenoate distributions within the euphotic zone of the eastern North Atlantic: correlation with production temperature. Deep Sea Research Part I: Oceanographic Research Papers, 40(10), 1935-1961, https://doi.org/10.1016/0967-0637(93)90040-A

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Abstract:
This paper reports the concentrations and within-class distributions of long-chain alkenones and alkyl alkenoates in the surface waters (0–50 m) of the eastern North Atlantic, and correlates their abundance and distribution with those of source organisms and with water temperature and other environmental variables. We collected these samples of >0.8 µm particulate material from the euphotic zone along the JGOFS 20°W longitude transect, from 61°N to 24°N, during seven cruises of the UK-JGOFS Biogeochemical Ocean Flux Study (BOFS) in 1989-1991; the biogeographical range of our 53 samples extends from the cold (<10°C), nutrient-rich and highly productive subarctic waters of the Iceland Basin to the warm (>25°C) oligotrophic subtropical waters off Africa. Surface water concentrations of total alkenone and alkenoates ranged from <50 ng/l in oligotrophic waters below 40°N to 2000-4500 ng/l in high latitude E. huxleyi blooms, and were well correlated with E. huxleyi cell densities, supporting the assumption that E. huxleyi is the predominant source of these compounds in the present day North Atlantic.
The within-class distribution of the C37 and C38 alkenones and C36 alkenoates varied strongly as a function of temperature, and was largely unaffected by nutrient concentration, bloom status and other surface water properties. The biosynthetic response of the source organisms to growth temperature differed between the cold (<16°C) waters above 47°N and the warmer waters to the south. In cold (<16°C) waters above 47°N, the relative amounts of alkenoates and C38 alkenones synthesized was a strong function of growth temperature, while the unsaturation ratio of the alkenones (C37 and C38) was uncorrelated with temperature. Conversely, in warm (>16°C) waters below 47°N, the relative proportions of alkenoates and alkenones synthesized remained constant with increasing temperature while the unsaturation ratios of the C37 and C38 methyl alkenones (Uk37 and Uk38Me, respectively) increased linearly. The fitted regressions of Uk37 and Uk38Me versus temperature for waters >16°C were both highly significant (r**2 > 0.96) and had identical slopes (0.057) that were 50% higher than the slope (0.034) of the temperature calibration of Uk37 reported by Prahl and Wakeham (1987; doi:10.1038/330367a0) over the same temperature range. These observations suggest either a physiological adjustment in biochemical response to growth temperature above a 16-17°C threshold and/or variation between different E. huxleyi strains and/or related species inhabiting the cold and warm water regions of the eastern North Atlantic.
Using our North Atlantic data set, we have produced multivariate temperature calibrations incorporating all major features of the alkenone and alkenoate data set. Predicted temperatures using multivariate calibrations are largely unbiased, with a standard error of approximately ±1°C over the entire data range. In contrast, simpler calibration models cannot adequately incorporate regional diversity and nonlinear trends with temperature. Our results indicate that calibrations based upon single variables, such as Uk37, can be strongly biased by unknown systematic errors arising from natural variability in the biosynthetic response of the source organisms to growth temperature. Multivariate temperature calibration can be expected to give more precise estimates of Integrated Production Temperatures (IPT) in the sedimentary record over a wider range of paleoenvironmental conditions, when derived using a calibration data set incorporating a similar range of natural variability in biosynthetic response.
Project(s):
Coverage:
Median Latitude: 49.925858 * Median Longitude: -19.526316 * South-bound Latitude: 24.455000 * West-bound Longitude: -22.583300 * North-bound Latitude: 61.281700 * East-bound Longitude: -14.833300
Date/Time Start: 1989-06-14T00:00:00 * Date/Time End: 1991-07-25T00:00:00
Minimum DEPTH, water: m * Maximum DEPTH, water: 50 m
Event(s):
CD46_PUMP1  * Latitude: 49.846700 * Longitude: -18.531700 * Date/Time: 1990-05-04T00:00:00 * Method/Device: Water pump (PUMP)
CD46_PUMP2  * Latitude: 48.896700 * Longitude: -17.016700 * Date/Time: 1990-05-17T00:00:00 * Method/Device: Water pump (PUMP)
CD47_PUMP1  * Latitude: 48.435000 * Longitude: -17.490000 * Date/Time: 1990-05-28T00:00:00 * Method/Device: Water pump (PUMP)
Size:
582 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Latitude

Longitude

Date/Time

Depth water [m]

Temp [°C]

C37:3Me [%]

Methyl hexatriaconta-7E 14E 21E-tri [%]

C37:2Me [%]
10 
Methyl hexatriaconta-14E 21E-die [%]
11 
Methyl hexatriaconta-14E 21E-die [%]
12 
C38:3Me [%]
13 
C38:2Et [%]
14 
C38:2Me [%]
15 
UK37
16 
AA36
D183_PUMP1 59.4150-20.98831989-06-14209.833.647.2610.7219.609.7211.225.752.080.2420.266
D183_PUMP2 59.6967-21.25331989-06-15510.221.3613.9618.2819.1912.709.153.941.420.4610.277
D183_PUMP3 59.6967-21.25331989-06-15410.228.2811.9817.2921.399.408.472.041.150.3790.282
D183_PUMP359.6967-21.25331989-06-15410.226.768.2811.3015.1317.5510.816.493.680.2990.422
D183_PUMP359.6967-21.25331989-06-151010.027.3713.0116.3217.4910.998.664.861.290.3740.265
D183_PUMP359.6967-21.25331989-06-15259.728.197.7114.0316.4811.7411.747.242.880.3320.327
D183_PUMP4 59.8000-21.16831989-06-162010.230.097.459.9521.2110.1911.207.182.740.2490.262
D183_PUMP459.8000-21.16831989-06-163010.022.948.2523.9516.3512.487.387.611.050.5110.338
D183_PUMP459.8000-21.16831989-06-16509.726.329.2710.1220.8612.879.658.432.500.2780.299
D183_PUMP5 55.9750-19.81831989-06-25411.720.175.8421.9419.0113.397.489.912.260.5210.352
D183_PUMP555.9750-19.81831989-06-251011.723.607.4821.0617.4712.916.628.702.170.4720.341
D183_PUMP555.9750-19.81831989-06-253011.620.629.8717.7418.1714.847.739.401.630.4620.346
D183_PUMP6 55.9800-19.92501989-06-263011.625.105.4416.7221.058.307.0511.364.980.4000.238
D183_PUMP7 51.9567-19.84501989-06-273014.019.038.4819.0712.1219.197.1710.304.640.5000.482
D183_PUMP8 51.8000-19.43331989-06-284012.424.834.5016.0417.0814.087.1613.083.240.3930.395
D183_PUMP9 46.9217-20.03501989-07-023014.522.621.8717.2413.4913.7412.8615.212.970.4310.474
D183_PUMP10 46.8400-20.03671989-07-02416.925.932.1122.266.0613.8711.9212.984.880.4620.628
D183_PUMP1046.8400-20.03671989-07-021515.528.690.9923.596.2414.549.6112.334.010.4520.668
D183_PUMP12 46.7533-19.86831989-07-071017.224.580.8420.146.7713.6412.2215.556.270.4500.642
CD46_PUMP1 49.8467-18.53171990-05-041512.427.013.2113.7216.8710.4413.0411.564.160.3370.342
CD46_PUMP2 48.8967-17.01671990-05-171512.925.614.1216.0216.5211.209.3413.104.100.3850.352
D191_PUMP1 48.4967-17.79831990-05-211013.926.193.0023.0111.5910.7411.069.524.890.4680.424
D191_PUMP2 48.4900-17.80331990-05-231013.721.413.5422.5714.9012.539.9612.812.290.5120.404
D191_PUMP3 48.4683-17.56171990-05-251014.321.942.8422.1313.4512.7310.4110.985.510.5020.439
D191_PUMP4 48.4483-17.49171990-05-271014.324.463.8221.5011.7512.4710.619.915.480.4690.445
CD47_PUMP1 48.4350-17.49001990-05-281014.626.682.8516.2313.4812.7210.8912.075.080.3780.438
CD47_PUMP2 48.2800-17.31331990-06-011014.926.113.7015.9214.4711.1410.6312.205.810.3790.380
CD47_PUMP248.2800-17.31331990-06-012512.525.233.5215.0316.7612.8710.3611.944.300.3730.388
CD47_PUMP3 47.9283-16.82331990-06-021014.926.522.9015.6314.9012.5910.4312.414.620.3710.414
CD53_PUMP1 47.0600-19.72671990-09-22417.426.311.3220.947.3010.9411.4014.357.440.4430.558
CD53_PUMP2 44.6550-20.56171990-09-22418.723.540.5727.475.567.619.3817.118.750.5390.554
CD53_PUMP3 47.8050-19.43671990-09-221018.023.090.6723.146.668.6411.0817.399.320.5010.541
CD53_PUMP347.8050-19.43671990-09-223018.023.541.9924.056.619.919.9215.718.270.5050.536
CD53_PUMP4 42.1617-21.46171990-09-23420.617.381.3230.225.0710.117.7416.9611.200.6350.613
CD53_PUMP5 41.1317-20.70501990-09-25420.914.090.8431.535.7810.546.7421.558.940.6910.615
CD53_PUMP6 42.1617-21.46171990-09-241020.714.973.1535.683.5716.174.7114.687.070.7040.706
CD53_PUMP7 38.7983-19.88671990-09-26421.615.703.3635.433.6912.865.3315.897.740.6930.648
CD53_PUMP8 35.1100-19.23831990-09-27422.79.437.4536.996.8318.162.9412.056.140.7970.560
CD53_PUMP9 32.9017-18.94171990-09-29423.47.633.8839.312.3610.414.0820.3911.930.8370.623
CD53_PUMP10 32.8650-19.29001990-09-30423.58.313.9238.282.8212.723.3519.6210.980.8220.653
CD53_PUMP11 32.4733-20.49331990-10-021024.96.3610.8634.672.8413.202.9718.7010.410.845
CD53_PUMP12 24.4550-20.40671990-10-081024.76.127.5842.832.1213.541.9917.028.800.8750.583
CD60_PUMP1 60.1667-20.00001991-06-20810.829.296.3310.9919.939.0813.576.953.860.2730.257
CD60_PUMP2 60.6667-22.58331991-06-22811.027.639.0011.5021.669.979.837.772.640.2940.245
CD60_PUMP3 60.4167-14.83331991-06-30512.522.095.2914.6719.6111.978.966.691.710.3990.325
CD61_PUMP1 61.0817-19.99171991-07-121012.325.015.4621.0319.2811.316.819.381.720.4570.314
CD61_PUMP2 61.2817-19.78501991-07-141512.425.414.9116.4220.718.887.8111.903.960.3930.257
CD61_PUMP3 60.5450-20.15331991-07-12412.324.315.2518.0719.6710.596.6512.353.110.4260.298
CD61_PUMP4 60.5483-19.54671991-07-12412.623.784.6419.1419.7310.936.7912.132.870.4460.310
CD61_PUMP5 60.7833-19.67831991-07-14413.125.675.8316.5519.4912.077.1210.113.160.3920.323
CD61_PUMP6 56.0600-19.97501991-07-25413.926.563.5114.7218.4611.0210.8810.414.430.3570.334
CD61_PUMP7 55.9300-20.01331991-07-25413.926.782.9315.9616.4110.2810.9211.375.350.3730.347
CD61_PUMP8 55.6283-20.00671991-07-25414.027.672.3015.3615.919.8812.1911.315.380.3570.352