Table 1 Core site, fractional abundance of individual isoprenoid GDGTs and TEX86 values
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2011
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| _version_ | 1867169038403108864 |
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| author | Ho, Sze Ling Yamamoto, Masanobu Mollenhauer, Gesine Minagawa, Masao |
| author_facet | Ho, Sze Ling Yamamoto, Masanobu Mollenhauer, Gesine Minagawa, Masao |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | TEXL86 and TEXH86 are organic palaeothermometers based on the lipids of Group 1 Crenarchaeota, recently proposed as a modified version of the original TEX86 index, but with significantly improved geographical coverage. Since few data from the global core top calibration are from the Pacific, this study was carried out to assess whether the global core top calibration is regionally biased or not. The result of principal components analysis of the fractional abundance of GDGTs, an analysis of variance (ANOVA) and the comparison of the residuals of TEXH 86 derived sea surface temperature (SST) estimates of the Pacific subset with that of the global data set suggest that the Pacific subset has a similar TEXH 86-SST relationship with the global data set. However, the regression line through the Pacific data and an ANOVA on the residuals of TEXL 86 derived SST estimates suggest otherwise. The contradictory findings are likely to stem from the large scatter in the Pacific TEXL 86 values in the mid temperature range. While regionality does not seem to exert a strong bias on TEXL 86 and TEXH 86 calibration, it appears that there is a strong need to resolve the large scatter in the global data set, especially in the mid and high latitudes, in order to improve the calibration for a better SST estimation. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_767415 |
| institution | PANGAEA |
| language | en |
| publishDate | 2011 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Table 1 Core site, fractional abundance of individual isoprenoid GDGTs and TEX86 values Ho, Sze Ling Yamamoto, Masanobu Mollenhauer, Gesine Minagawa, Masao Acyclic glycerol dialkyl glycerol tetraether, fractional abundance; Campaign of event; Crenarchaeol, fractional abundance; Crenarchaeol regio-isomer, fractional abundance; DEPTH, sediment/rock; Dicyclic glycerol dialkyl glycerol tetraether, fractional abundance; Elevation of event; Event label; GC; Gravity corer; Hakuho-Maru; HY03; HY04; HY05; HY06; HY07; HY08; HY08B; HY09; KH-01-3; KH-01-3-01; KH-01-3-08; KH-01-3-10; KH-01-3-17; KH-01-3-19; KH-03-1; KH-04-5; Latitude of event; Longitude of event; Monocyclic glycerol dialkyl glycerol tetraether, fractional abundance; Pacific Ocean; PC; Piston corer; SX02; SX09; SX10; SX14; SX15; SX16; SX17; Temperature, water, interpolated; Tetraether index of 86 carbon atoms; Tricyclic glycerol dialkyl glycerol tetraether, fractional abundance TEXL86 and TEXH86 are organic palaeothermometers based on the lipids of Group 1 Crenarchaeota, recently proposed as a modified version of the original TEX86 index, but with significantly improved geographical coverage. Since few data from the global core top calibration are from the Pacific, this study was carried out to assess whether the global core top calibration is regionally biased or not. The result of principal components analysis of the fractional abundance of GDGTs, an analysis of variance (ANOVA) and the comparison of the residuals of TEXH 86 derived sea surface temperature (SST) estimates of the Pacific subset with that of the global data set suggest that the Pacific subset has a similar TEXH 86-SST relationship with the global data set. However, the regression line through the Pacific data and an ANOVA on the residuals of TEXL 86 derived SST estimates suggest otherwise. The contradictory findings are likely to stem from the large scatter in the Pacific TEXL 86 values in the mid temperature range. While regionality does not seem to exert a strong bias on TEXL 86 and TEXH 86 calibration, it appears that there is a strong need to resolve the large scatter in the global data set, especially in the mid and high latitudes, in order to improve the calibration for a better SST estimation. |
| title | Table 1 Core site, fractional abundance of individual isoprenoid GDGTs and TEX86 values |
| topic | Acyclic glycerol dialkyl glycerol tetraether, fractional abundance; Campaign of event; Crenarchaeol, fractional abundance; Crenarchaeol regio-isomer, fractional abundance; DEPTH, sediment/rock; Dicyclic glycerol dialkyl glycerol tetraether, fractional abundance; Elevation of event; Event label; GC; Gravity corer; Hakuho-Maru; HY03; HY04; HY05; HY06; HY07; HY08; HY08B; HY09; KH-01-3; KH-01-3-01; KH-01-3-08; KH-01-3-10; KH-01-3-17; KH-01-3-19; KH-03-1; KH-04-5; Latitude of event; Longitude of event; Monocyclic glycerol dialkyl glycerol tetraether, fractional abundance; Pacific Ocean; PC; Piston corer; SX02; SX09; SX10; SX14; SX15; SX16; SX17; Temperature, water, interpolated; Tetraether index of 86 carbon atoms; Tricyclic glycerol dialkyl glycerol tetraether, fractional abundance |
| url | https://doi.org/10.1594/PANGAEA.767415 |