Organic Carbon Remineralization and Calcium Carbonate Production Rates in the Red Sea Computed From Oxygen and Alkalinity Utilizations

IF 3.7 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Salma Elageed, Abdirahman M. Omar, Emil Jeansson, Ingunn Skjelvan, Knut Barthel, Truls Johannessen
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Abstract

Organic carbon remineralization rate (OCRR) and the calcium carbonate production rate (CCPR) are influential variables on the efficiency of the biological carbon pump (BCP) but are not well understood in Red Sea. We used historical cruise data of carbonate chemistry, oxygen, and transient tracers from five locations along the north–south central axis of the Red Sea to estimate OCRR and CCPR from tracer-based water mean ages (Γ), apparent oxygen utilization (AOU), and alkalinity utilization (AU). This resulted in the first basin-wide and depth-resolving (100–1,000 m) OCRR and CCPR estimates. Spatial distributions for Γ, AOU, and AU were strongly influenced by the large-scale circulation and showed maxima intermediate depths (400–500 m). Conversely, OCRR and CCPR showed no statistically significant latitudinal differences and peaked (6.5 ± 4.3 and 11.9 ± 4.6 mmol C m−3 yr−1, respectively) at 100-m depth, which decreased to nearly constant values (3.8 ± 0.7 and 1.4 ± 0.3 mmol C m−3 yr−1, respectively) at 300 m and deeper. By depth-integrating CCPR, we estimated annual calcium carbonate production (CCP) of (0.8 ± 0.3) × 1012 mol, or 0.6% of global ocean production, in the Red Sea, which has only 0.12% of the world ocean area. High correlation between AU and Γ indicated in situ alkalinity removal taking place also in subsurface and deep waters, probably due to chemical precipitation, which has been previously reported for the area. CCP-induced AU affects the carbonate chemistry in the Red Sea water column, and we hypothesize that it also impacts that of the Gulf of Aden through the outflowing Red Sea Outflow Water.

从氧和碱度利用计算红海有机碳再矿化和碳酸钙产量
有机碳再矿化率(OCRR)和碳酸钙产率(CCPR)是影响生物碳泵(BCP)效率的重要因素,但在红海海域尚未得到很好的认识。我们利用红海南北中轴线上五个地点的碳酸盐化学、氧和瞬态示踪剂的历史航行数据,通过示踪剂为基础的水平均年龄(Γ)、表观氧利用率(AOU)和碱度利用率(AU)来估计ocr和CCPR。这产生了第一个盆地宽度和深度分辨率(100-1,000 m)的ocr和CCPR估计。Γ、AOU和AU的空间分布受大尺度环流的强烈影响,在中间深度(400 ~ 500 m)处最大,而OCRR和CCPR在100 m处无显著的纬度差异,峰值分别为6.5±4.3和11.9±4.6 mmol C m−3 yr−1,在300 m及更深处降至接近恒定值(3.8±0.7和1.4±0.3 mmol C m−3 yr−1)。通过深度积分CCPR,我们估计红海的碳酸钙年产量(CCP)为(0.8±0.3)× 1012 mol,占全球海洋产量的0.6%,而红海仅占世界海洋面积的0.12%。AU和Γ之间的高度相关性表明,在地下和深水中也发生了原位碱度去除,可能是由于化学沉淀,这是以前在该地区报道过的。ccp诱导AU影响红海水体中的碳酸盐化学,我们假设它也通过红海流出水影响亚丁湾的碳酸盐化学。
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来源期刊
Journal of Geophysical Research: Biogeosciences
Journal of Geophysical Research: Biogeosciences Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
5.40%
发文量
242
期刊介绍: JGR-Biogeosciences focuses on biogeosciences of the Earth system in the past, present, and future and the extension of this research to planetary studies. The emerging field of biogeosciences spans the intellectual interface between biology and the geosciences and attempts to understand the functions of the Earth system across multiple spatial and temporal scales. Studies in biogeosciences may use multiple lines of evidence drawn from diverse fields to gain a holistic understanding of terrestrial, freshwater, and marine ecosystems and extreme environments. Specific topics within the scope of the section include process-based theoretical, experimental, and field studies of biogeochemistry, biogeophysics, atmosphere-, land-, and ocean-ecosystem interactions, biomineralization, life in extreme environments, astrobiology, microbial processes, geomicrobiology, and evolutionary geobiology
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