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DOI | https://doi.org/10.1594/PANGAEA.874268 |
Particle export fluxes to the oxygen minimum zone of the eastern tropical North Atlantic | |
Engel; Anja; Wagner; Hannes; Le Moigne; Frédéric A C; Wilson; Samuel T | |
发布日期 | 2017-04-04 |
数据集类型 | dataset |
英文简介 | In the ocean, sinking of particulate organic mat- ter (POM) drives carbon export from the euphotic zone and supplies nutrition to mesopelagic communities, the feeding and degradation activities of which in turn lead to export flux attenuation. Oxygen (O2) minimum zones (OMZs) with suboxic water layers (< 5 µmol O2 kg-1 ) show a lower carbon flux attenuation compared to well- oxygenated waters (> 100 µmol O2 kg-1), supposedly due to reduced heterotrophic activity. This study focuses on sinking particle fluxes through hypoxic mesopelagic waters (< 60 µmol O2 kg-1); these represent about 100 times more ocean volume globally compared to suboxic waters, but they have less been studied. Particle export fluxes and attenuation coefficients were determined in the eastern tropical North Atlantic (ETNA) using two surface-tethered drifting sediment trap arrays with seven trapping depths located between 100 and 600 m. |
空间范围 | Median Latitude: 10.124915 * Median Longitude: -20.999915 * South-bound Latitude: 10.000000 * West-bound Longitude: -21.000000 * North-bound Latitude: 10.249830 * East-bound Longitude: -20.999830 |
时间范围 | 2014-03-24T09:02:00 - 2014-03-27T14:01:00 |
语种 | 英语 |
国家 | 国际 |
学科大类 | 气候变化 |
学科子类 | 气候变化 |
文献类型 | 数据集 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/215333 |
推荐引用方式 GB/T 7714 | Engel,Anja,Wagner,et al. Particle export fluxes to the oxygen minimum zone of the eastern tropical North Atlantic.2017-04-04.https://doi.org/10.1594/PANGAEA.874268. |
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