(Table 2) Radiocarbon data (fMC; fraction modern carbon and conventional 14C ages) of foraminifera, TOC and alkenones of cores ME0005A-24JC, Y69-71P and MC16
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2010
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| _version_ | 1867169969021648896 |
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| author | Kusch, Stephanie Eglinton, Timothy Ian Mix, Alan C Mollenhauer, Gesine |
| author_facet | Kusch, Stephanie Eglinton, Timothy Ian Mix, Alan C Mollenhauer, Gesine |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Paired radiocarbon measurements on haptophyte biomarkers (alkenones) and on co-occurring tests of planktic foraminifera (Neogloboquadrina dutertrei and Globogerinoides sacculifer) from late glacial to Holocene sediments at core locations ME0005-24JC, Y69-71P, and MC16 from the south-western and central Panama Basin indicate no significant addition of pre-aged alkenones by lateral advection. The strong temporal correspondence between alkenones, foraminifera and total organic carbon (TOC) also implies negligible contributions of aged terrigenous material. Considering controversial evidence for sediment redistribution in previous studies of these sites, our data imply that the laterally supplied material cannot stem from remobilization of substantially aged sediments. Transport, if any, requires syn-depositional nepheloid layer transport and redistribution of low-density or fine-grained components within decades of particle formation. Such rapid and local transport minimizes the potential for temporal decoupling of proxies residing in different grain-size fractions and thus facilitates comparison of various proxies for paleoceanographic reconstructions in this study area. Anomalously old foraminiferal tests from a glacial depth interval of core Y69-71P may result from episodic spillover of fast bottom currents across the Carnegie Ridge transporting foraminiferal sands towards the north. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_735532 |
| institution | PANGAEA |
| language | en |
| publishDate | 2010 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 2) Radiocarbon data (fMC; fraction modern carbon and conventional 14C ages) of foraminifera, TOC and alkenones of cores ME0005A-24JC, Y69-71P and MC16 Kusch, Stephanie Eglinton, Timothy Ian Mix, Alan C Mollenhauer, Gesine Age, 14C AMS; Age, dated; Age, dated, standard deviation; Age, dated material; Center for Marine Environmental Sciences; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Depth comment; Event label; Fraction modern carbon; Fraction modern carbon, standard deviation; GC; Gravity corer; Knorr; KNR182-9; MARUM; MC16; ME0005A; ME0005A-24JC; Melville; NEMO; North Pacific Ocean; Panama Basin; PC; Piston corer; Reference/source; Y69-71P; YALOC69; Yaquina Paired radiocarbon measurements on haptophyte biomarkers (alkenones) and on co-occurring tests of planktic foraminifera (Neogloboquadrina dutertrei and Globogerinoides sacculifer) from late glacial to Holocene sediments at core locations ME0005-24JC, Y69-71P, and MC16 from the south-western and central Panama Basin indicate no significant addition of pre-aged alkenones by lateral advection. The strong temporal correspondence between alkenones, foraminifera and total organic carbon (TOC) also implies negligible contributions of aged terrigenous material. Considering controversial evidence for sediment redistribution in previous studies of these sites, our data imply that the laterally supplied material cannot stem from remobilization of substantially aged sediments. Transport, if any, requires syn-depositional nepheloid layer transport and redistribution of low-density or fine-grained components within decades of particle formation. Such rapid and local transport minimizes the potential for temporal decoupling of proxies residing in different grain-size fractions and thus facilitates comparison of various proxies for paleoceanographic reconstructions in this study area. Anomalously old foraminiferal tests from a glacial depth interval of core Y69-71P may result from episodic spillover of fast bottom currents across the Carnegie Ridge transporting foraminiferal sands towards the north. |
| title | (Table 2) Radiocarbon data (fMC; fraction modern carbon and conventional 14C ages) of foraminifera, TOC and alkenones of cores ME0005A-24JC, Y69-71P and MC16 |
| topic | Age, 14C AMS; Age, dated; Age, dated, standard deviation; Age, dated material; Center for Marine Environmental Sciences; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Depth comment; Event label; Fraction modern carbon; Fraction modern carbon, standard deviation; GC; Gravity corer; Knorr; KNR182-9; MARUM; MC16; ME0005A; ME0005A-24JC; Melville; NEMO; North Pacific Ocean; Panama Basin; PC; Piston corer; Reference/source; Y69-71P; YALOC69; Yaquina |
| url | https://doi.org/10.1594/PANGAEA.735532 |