Caromel, Aude G M; Schmidt, Daniela N; Phillips, J C; Rayfield, Emily J (2014): Northwards and eastwards velocities extracted from a historical run (for the year 2000) of the UVic Earth System Climate Model of Weaver et al. (2001) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.829780, In: Caromel, AGM et al. (2014): Current velocities and settling experimental results [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.829781
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
This study provides a theoretical assessment of the potential bias due to differential lateral transport on multi-proxy studies based on a range of marine microfossils. Microfossils preserved in marine sediments are at the centre of numerous proxies for paleoenvironmental reconstructions. The precision of proxies is based on the assumption that they accurately represent the overlying watercolumn properties and faunas. Here we assess the possibility of a syn-depositional bias in sediment assemblages caused by horizontal drift in the water column, due to differential settling velocities of sedimenting particles based on their shape, size and density, and due to differences in current velocities. Specifically we calculate the post-mortem lateral transport undergone by planktic foraminifera and a range of other biological proxy carriers (diatoms, radiolaria and fecal pellets transporting coccolithophores) in several regions with high current velocities. We find that lateral transport of different planktic foraminiferal species is minimal due to high settling velocities. No significant shape- or size-dependent sorting occurs before reaching the sediment, making planktic foraminiferal ideal proxy carriers. In contrast, diatoms, radiolaria and fecal pellets can be transported up to 500km in some areas. For example in the Agulhas current, transport can lead to differences of up to 2°C in temperature reconstructions between different proxies in response to settling velocities. Therefore, sediment samples are likely to contain different proportions of local and imported particles, decreasing the precision of proxies based on these groups and the accuracy of the temperature reconstruction.
Related to:
Caromel, Aude G M; Schmidt, Daniela N; Phillips, J C; Rayfield, Emily J (submitted): Repercussions of post-mortem differential settling on sediment assemblages and multi-proxy paleo-reconstructions. data submission http://issues.pangaea.de/browse/PDI-7133, Paleoceanography
Weaver, Andrew; Eby, Michael; Wiebe, Edward C; Bitz, Cecilia M; Duffy, Phil B; Ewen, Tracy L; Holland, Marika M; MacFadyen, Amy; Matthews, H Damon; Meissner, Katrin J; Saenko, Oleg; Schmittner, Andreas; Wang, Huaxiao; Yoshimori, Masakazu (2001): The UVic earth system climate model: Model description, climatology, and applications to past, present and future climates. Atmosphere-Ocean, 39(4), 361-428, https://doi.org/10.1080/07055900.2001.9649686
Coverage:
Median Latitude: -8.178261 * Median Longitude: 36.078261 * South-bound Latitude: -32.400000 * West-bound Longitude: -75.600000 * North-bound Latitude: 34.200000 * East-bound Longitude: 136.800000
Minimum DEPTH, water: 25 m * Maximum DEPTH, water: 2390 m
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Current | Current | Caromel, Aude G M | |||
| 2 | LATITUDE | Latitude | Geocode | |||
| 3 | LONGITUDE | Longitude | Geocode | |||
| 4 | DEPTH, water | Depth water | m | Geocode | ||
| 5 | Depth, top/min | Depth top | m | Caromel, Aude G M | ||
| 6 | Depth, bottom/max | Depth bot | m | Caromel, Aude G M | ||
| 7 | Velocity, compressional wave along X-axis | Vp X | m/s | Caromel, Aude G M | ||
| 8 | Velocity, compressional wave along Y-axis | Vp Y | m/s | Caromel, Aude G M |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
460 data points
Data
| 1 Current | 2 Latitude | 3 Longitude | 4 Depth water [m] | 5 Depth top [m] | 6 Depth bot [m] | 7 Vp X [m/s] | 8 Vp Y [m/s] |
|---|---|---|---|---|---|---|---|
| Benguela | -19.8 | 7.2 | 25 | 0 | 50 | -0.02990 | -0.00406 |
| Benguela | -19.8 | 7.2 | 90 | 50 | 130 | -0.00317 | 0.01510 |
| Benguela | -19.8 | 7.2 | 185 | 130 | 240 | -0.00444 | 0.00847 |
| Benguela | -19.8 | 7.2 | 310 | 240 | 380 | -0.00079 | 0.00082 |
| Benguela | -19.8 | 7.2 | 465 | 380 | 550 | 0.00052 | -0.00041 |
| Benguela | -19.8 | 7.2 | 650 | 550 | 750 | 0.00060 | -0.00061 |
| Benguela | -19.8 | 7.2 | 865 | 750 | 980 | 0.00061 | -0.00046 |
| Benguela | -19.8 | 7.2 | 1110 | 980 | 1240 | 0.00018 | -0.00007 |
| Benguela | -19.8 | 7.2 | 1385 | 1240 | 1530 | -0.00014 | 0.00016 |
| Benguela | -19.8 | 7.2 | 1690 | 1530 | 1850 | -0.00020 | -0.00008 |
| Benguela | -19.8 | 7.2 | 2025 | 1850 | 2200 | 0.00023 | 0.00024 |
| Gulf Stream | 30.6 | -75.6 | 25 | 0 | 50 | 0.05660 | 0.20100 |
| Gulf Stream | 30.6 | -75.6 | 90 | 50 | 130 | 0.05160 | 0.19700 |
| Gulf Stream | 30.6 | -75.6 | 185 | 130 | 240 | 0.04250 | 0.17400 |
| Gulf Stream | 30.6 | -75.6 | 310 | 240 | 380 | 0.02580 | 0.12700 |
| Gulf Stream | 30.6 | -75.6 | 465 | 380 | 550 | 0.01130 | 0.08060 |
| Gulf Stream | 30.6 | -75.6 | 650 | 550 | 750 | 0.02980 | 0.04650 |
| Gulf Stream | 30.6 | -75.6 | 865 | 750 | 980 | -0.00459 | 0.01930 |
| Kuroshio | 30.6 | 136.8 | 25 | 0 | 50 | 0.14700 | 0.00219 |
| Kuroshio | 30.6 | 136.8 | 90 | 50 | 130 | 0.14000 | 0.00838 |
| Kuroshio | 30.6 | 136.8 | 185 | 130 | 240 | 0.11900 | 0.00901 |
| Kuroshio | 30.6 | 136.8 | 310 | 240 | 380 | 0.09840 | 0.00866 |
| Kuroshio | 30.6 | 136.8 | 465 | 380 | 550 | 0.07410 | 0.00798 |
| Kuroshio | 30.6 | 136.8 | 650 | 550 | 750 | 0.03570 | 0.00648 |
| Kuroshio | 30.6 | 136.8 | 865 | 750 | 980 | 0.00619 | 0.00436 |
| Kuroshio | 30.6 | 136.8 | 1110 | 980 | 1240 | 0.00061 | 0.00206 |
| Kuroshio | 30.6 | 136.8 | 1385 | 1240 | 1530 | 0.00188 | 0.00084 |
| Kuroshio | 30.6 | 136.8 | 1690 | 1530 | 1850 | 0.00099 | 0.00102 |
| Kuroshio | 30.6 | 136.8 | 2025 | 1850 | 2200 | 0.00197 | 0.00088 |
| Agulhas | 34.2 | 32.4 | 25 | 0 | 50 | -0.00050 | -0.11300 |
| Agulhas | 34.2 | 32.4 | 90 | 50 | 130 | -0.06060 | -0.11200 |
| Agulhas | 34.2 | 32.4 | 185 | 130 | 240 | -0.06300 | -0.10300 |
| Agulhas | 34.2 | 32.4 | 310 | 240 | 380 | -0.05770 | -0.08760 |
| Agulhas | 34.2 | 32.4 | 465 | 380 | 550 | -0.04700 | -0.07100 |
| Agulhas | 34.2 | 32.4 | 650 | 550 | 750 | -0.03420 | -0.05480 |
| Agulhas | 34.2 | 32.4 | 865 | 750 | 980 | -0.02120 | -0.03780 |
| Agulhas | 34.2 | 32.4 | 1110 | 980 | 1240 | -0.01170 | -0.02350 |
| Agulhas | 34.2 | 32.4 | 1385 | 1240 | 1530 | -0.00782 | -0.01290 |
| Agulhas | 34.2 | 32.4 | 1690 | 1530 | 1850 | -0.00546 | -0.00543 |
| Agulhas | 34.2 | 32.4 | 2025 | 1850 | 2200 | -0.00379 | 0.00007 |
| Agulhas | 34.2 | 32.4 | 2390 | 2200 | 2580 | -0.00260 | 0.00141 |
| Agulhas | -32.4 | 36.0 | 90 | 50 | 130 | -0.10700 | -0.21100 |
| Agulhas | -32.4 | 36.0 | 185 | 130 | 240 | -0.11100 | -0.20600 |
| Agulhas | -32.4 | 36.0 | 310 | 240 | 380 | -0.10300 | -0.18600 |
| Agulhas | -32.4 | 36.0 | 465 | 380 | 550 | -0.08380 | -0.15200 |
| Agulhas | -32.4 | 36.0 | 650 | 550 | 750 | -0.06210 | -0.10600 |
| Agulhas | -32.4 | 36.0 | 865 | 750 | 980 | -0.04200 | -0.05590 |
| Agulhas | -32.4 | 36.0 | 1110 | 980 | 1240 | -0.02600 | -0.01760 |
| Agulhas | -32.4 | 36.0 | 1385 | 1240 | 1530 | -0.01710 | -0.00172 |
| Agulhas | -32.4 | 36.0 | 1690 | 1530 | 1850 | -0.00771 | -0.00002 |
| Agulhas | -32.4 | 36.0 | 2025 | 1850 | 2200 | 0.00081 | 0.00273 |
| Agulhas | -32.4 | 36.0 | 2390 | 2200 | 2580 | 0.00368 | 0.00496 |
| Agulhas | -30.6 | 36.0 | 90 | 50 | 130 | -0.03570 | -0.22400 |
| Agulhas | -30.6 | 36.0 | 185 | 130 | 240 | -0.04790 | -0.21300 |
| Agulhas | -30.6 | 36.0 | 310 | 240 | 380 | -0.05480 | -0.18600 |
| Agulhas | -30.6 | 36.0 | 465 | 380 | 550 | -0.05220 | -0.15200 |
| Agulhas | -30.6 | 36.0 | 650 | 550 | 750 | -0.04020 | -0.11400 |
| Agulhas | -30.6 | 36.0 | 865 | 750 | 980 | -0.02430 | -0.07300 |
| Agulhas | -30.6 | 36.0 | 1110 | 980 | 1240 | -0.01500 | -0.03780 |
| Agulhas | -30.6 | 36.0 | 1385 | 1240 | 1530 | -0.01620 | -0.01540 |
| Agulhas | -30.6 | 36.0 | 1690 | 1530 | 1850 | -0.01100 | -0.00286 |
| Agulhas | -30.6 | 36.0 | 2025 | 1850 | 2200 | -0.00341 | 0.00207 |
| Agulhas | -30.6 | 36.0 | 2390 | 2200 | 2580 | -0.00187 | 0.00267 |
| Agulhas | -28.8 | 36.0 | 90 | 50 | 130 | -0.00367 | -0.16600 |
| Agulhas | -28.8 | 36.0 | 185 | 130 | 240 | -0.01980 | -0.15400 |
| Agulhas | -28.8 | 36.0 | 310 | 240 | 380 | -0.03030 | -0.12800 |
| Agulhas | -28.8 | 36.0 | 465 | 380 | 550 | -0.03020 | -0.10100 |
| Agulhas | -28.8 | 36.0 | 650 | 550 | 750 | -0.02460 | -0.07730 |
| Agulhas | -28.8 | 36.0 | 865 | 750 | 980 | -0.01740 | -0.05440 |
| Agulhas | -28.8 | 36.0 | 1110 | 980 | 1240 | -0.00739 | -0.03750 |
| Agulhas | -28.8 | 36.0 | 1385 | 1240 | 1530 | 0.00000 | 0.00000 |
| Agulhas | -28.8 | 36.0 | 1690 | 1530 | 1850 | 0.00000 | 0.00000 |
| Agulhas | -28.8 | 36.0 | 2025 | 1850 | 2200 | 0.00000 | 0.00000 |
| Agulhas | -28.8 | 36.0 | 2390 | 2200 | 2580 | 0.00000 | 0.00000 |
| Agulhas | -27.0 | 36.0 | 25 | 0 | 50 | -0.00404 | -0.13100 |
| Agulhas | -27.0 | 36.0 | 90 | 50 | 130 | -0.01600 | -0.12000 |
| Agulhas | -27.0 | 36.0 | 185 | 130 | 240 | -0.02530 | -0.09730 |
| Agulhas | -27.0 | 36.0 | 310 | 240 | 380 | -0.02540 | -0.07470 |
| Agulhas | -27.0 | 36.0 | 465 | 380 | 550 | -0.01440 | -0.05910 |
| Agulhas | -27.0 | 36.0 | 650 | 550 | 750 | -0.00344 | -0.04710 |
| Agulhas | -27.0 | 36.0 | 865 | 750 | 980 | 0.00066 | -0.03860 |
| Agulhas | -27.0 | 39.6 | 90 | 50 | 130 | -0.02840 | -0.00197 |
| Agulhas | -27.0 | 39.6 | 185 | 130 | 240 | -0.05110 | -0.01430 |
| Agulhas | -27.0 | 39.6 | 310 | 240 | 380 | -0.07040 | -0.01870 |
| Agulhas | -27.0 | 39.6 | 465 | 380 | 550 | -0.07010 | -0.01470 |
| Agulhas | -27.0 | 39.6 | 650 | 550 | 750 | -0.04830 | -0.00461 |
| Agulhas | -27.0 | 39.6 | 865 | 750 | 980 | -0.02080 | 0.00394 |
| Agulhas | -27.0 | 39.6 | 1110 | 980 | 1240 | -0.07230 | 0.00947 |
| Agulhas | -27.0 | 39.6 | 1385 | 1240 | 1530 | -0.00389 | 0.00793 |
| Agulhas | -27.0 | 39.6 | 1690 | 1530 | 1850 | -0.00073 | 0.00191 |
| Agulhas | -27.0 | 39.6 | 2025 | 1850 | 2200 | 0.00073 | 0.00144 |
| Agulhas | -27.0 | 39.6 | 2390 | 2200 | 2580 | 0.00070 | 0.00237 |