Richey, J E; Hollander, David J; Flower, Benjamin P; Eglinton, Timothy Ian (2011): (Table S1) TEX86 and BIT record from sediment core PBBC-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.827381, Supplement to: Richey, JE et al. (2011): Merging late Holocene molecular organic and foraminiferal-based geochemical records of sea surface temperature in the Gulf of Mexico. Paleoceanography, 26(1), PA1209, https://doi.org/10.1029/2010PA002000
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Abstract:
A molecular organic geochemical proxy (TEX86) for sea surface temperature (SST) is compared with a foraminifera-based SST proxy (Mg/Ca) in a decadal-resolution marine sedimentary record spanning the last 1000 years from the Gulf of Mexico. We assess the relative strengths of the organic and inorganic paleoceanographic techniques for reconstructing high-resolution SST variability during recent climate events, including the Little Ice Age (LIA) and the Medieval Warm Period (MWP). SST estimates based on the molecular organic proxy TEX86 show a similar magnitude and pattern of SST variability to foraminiferal Mg/Ca-SST estimates but with some important differences. For instance, both proxies show a cooling (1°C-2°C) of Gulf of Mexico SSTs during the LIA. During the MWP, however, Mg/Ca-SSTs are similar to near-modern SSTs, while TEX86 indicates SSTs that were cooler than modern. Using the respective SST calibrations for each proxy results in TEX86-SST estimates that are 2°C-4°C warmer than Mg/Ca-SST throughout the 1000 year record. We interpret the TEX86-SST as a summer-weighted SST signal from the upper mixed layer, whereas the Mg/Ca-SST better reflects the mean annual SST. Downcore differences in the SST estimates between the two proxies (DeltaT = TEX86 - Mg/Ca) are interpreted in the context of varying seasonality and/or changing water column temperature gradients.
Coverage:
Latitude: 27.193500 * Longitude: -91.409000
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 1.082 m
Event(s):
PBBC-1 * Latitude: 27.193500 * Longitude: -91.409000 * Elevation: -2259.0 m * Location: Pigmy Basin * Method/Device: Box corer (BC)
Comment:
Each raw TEX86 and BIT index value represents the mean of 3-6 measurements per sample.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Tetraether index of 86 carbon atoms | TEX86 | Richey, J E | |||
3 | Branched and isoprenoid tetraether index | BIT | Richey, J E |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
174 data points
Data
1 Depth sed [m] | 2 TEX86 | 3 BIT |
---|---|---|
0.000 | 0.700 | 0.144 |
0.012 | 0.691 | 0.149 |
0.025 | 0.698 | 0.181 |
0.049 | 0.691 | 0.206 |
0.062 | 0.679 | 0.264 |
0.074 | 0.690 | 0.237 |
0.086 | 0.696 | 0.147 |
0.098 | 0.686 | 0.272 |
0.111 | 0.684 | 0.293 |
0.123 | 0.686 | 0.276 |
0.135 | 0.671 | 0.347 |
0.148 | 0.671 | 0.305 |
0.160 | 0.676 | 0.268 |
0.172 | 0.688 | 0.270 |
0.184 | 0.667 | 0.269 |
0.197 | 0.683 | 0.257 |
0.209 | 0.681 | 0.269 |
0.221 | 0.678 | 0.278 |
0.234 | 0.680 | 0.295 |
0.246 | 0.676 | 0.308 |
0.258 | 0.669 | 0.313 |
0.271 | 0.675 | 0.313 |
0.283 | 0.678 | 0.317 |
0.295 | 0.676 | 0.321 |
0.308 | 0.681 | 0.329 |
0.320 | 0.675 | 0.338 |
0.332 | 0.679 | 0.308 |
0.344 | 0.677 | 0.265 |
0.357 | 0.671 | 0.263 |
0.369 | 0.689 | 0.238 |
0.381 | 0.680 | 0.194 |
0.394 | 0.686 | 0.199 |
0.406 | 0.681 | 0.202 |
0.418 | 0.685 | 0.213 |
0.430 | 0.674 | 0.218 |
0.443 | 0.681 | 0.220 |
0.455 | 0.690 | 0.228 |
0.467 | 0.683 | 0.199 |
0.480 | 0.680 | 0.208 |
0.492 | 0.685 | 0.219 |
0.504 | 0.686 | 0.216 |
0.517 | 0.682 | 0.226 |
0.529 | 0.685 | 0.236 |
0.541 | 0.683 | 0.176 |
0.554 | 0.678 | 0.230 |
0.566 | 0.676 | 0.214 |
0.578 | 0.681 | 0.227 |
0.603 | 0.679 | 0.202 |
0.615 | 0.673 | 0.217 |
0.627 | 0.657 | 0.245 |
0.640 | 0.669 | 0.243 |
0.652 | 0.673 | 0.227 |
0.664 | 0.664 | 0.287 |
0.676 | 0.683 | 0.345 |
0.689 | 0.666 | 0.298 |
0.701 | 0.679 | 0.211 |
0.713 | 0.677 | 0.178 |
0.726 | 0.674 | 0.155 |
0.738 | 0.677 | 0.167 |
0.750 | 0.672 | 0.215 |
0.763 | 0.663 | 0.251 |
0.775 | 0.677 | 0.237 |
0.787 | 0.668 | 0.229 |
0.800 | 0.677 | 0.212 |
0.812 | 0.679 | 0.230 |
0.824 | 0.663 | 0.255 |
0.836 | 0.683 | 0.255 |
0.849 | 0.667 | 0.338 |
0.861 | 0.676 | 0.368 |
0.873 | 0.672 | 0.266 |
0.886 | 0.657 | 0.256 |
0.898 | 0.663 | 0.269 |
0.910 | 0.665 | 0.262 |
0.922 | 0.654 | 0.306 |
0.935 | 0.658 | 0.324 |
0.947 | 0.652 | 0.288 |
0.959 | 0.650 | 0.271 |
0.972 | 0.672 | 0.239 |
0.984 | 0.663 | 0.160 |
0.996 | 0.672 | 0.146 |
1.009 | 0.666 | 0.171 |
1.021 | 0.681 | 0.196 |
1.033 | 0.674 | 0.212 |
1.046 | 0.672 | 0.212 |
1.058 | 0.665 | 0.215 |
1.070 | 0.668 | 0.192 |
1.082 | 0.663 | 0.201 |