量化硅酸盐和溶解氮在共同限制孟加拉湾幼发区初级和次级生产力中的作用

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Inakonda Veera Ganga Bhavani, Faseela Hamza, B. R. Smitha, Vinu Valsala
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引用次数: 0

摘要

基于了解区域海洋学的北太平洋生态系统模式(NEMURO)的单柱物理和生物耦合模式与氮和硅循环适用于孟加拉湾(BoB)环境。该模型模拟了东西孟加拉湾(2016 年至 2017 年)沿 Bio-Argos 航迹的浮游生物量和营养物质,并与观测结果进行了验证。模型合理地模拟了亚表层叶绿素最高点(SCM)的常年结构。此外,还进行了三次实验,以了解开阔洋 BoB 在氮(NO3 + NH4)和硅酸盐(Si(OH)4)方面的初级和次级生产限制。在 "无 NO3 "实验中,硝酸盐限制项[即 NO3/(NO3 + KNO3)]被设为零,这样,与对照情况的差异就给出了 "再生产 "在初级和次级总产量中的作用。同样,还进行了无 NH4 实验,以推断 "新产量 "的作用。新生物量(再生生物量)占开阔洋博波东部生物量的 85 ± 1%(28 ± 6%)。西区的相应数值为 86 ± 1% (42 ± 2%)。在初级生产者中,新(再生)生产在东博波占 72 ± 1%(24 ± 6%),在西博波占 74 ± 1%(37 ± 2%)。硅酸盐限制了东博波(西博波)硅藻的生产,占硅藻实际数量的 46% ± 22% (45% ± 27%)。从地表到 60 米深处,我们观察到东渤海的硝酸盐限制很严重,而西渤海从 6 月到 9 月的硝酸盐和硅酸盐限制相同;其余月份,这两个区域的硝酸盐限制均为中等。这项研究表明,与硅酸盐相比,硝酸盐似乎是东渤海和西渤海表面的限制性营养元素。由于硅质线比硝质线更深,因此在所有季节,硅酸盐都是渤海 65 米至 105 米深处的潜在限制性营养元素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Quantifying the Role of Silicate and Dissolved Nitrogen in Co-Limiting the Primary and Secondary Productivity of the Bay of Bengal Euphotic Zone

A single-column coupled physical and biological model based on the North Pacific Ecosystem Model for Understanding Regional Oceanography (NEMURO) with nitrogen and silicon cycles is adapted for the Bay of Bengal (BoB) environment. The model simulated plankton biomass and nutrients along the track of Bio-Argos over East and West BoB (from 2016 to 2017) are validated with the observations. The model reasonably simulates the perennial structure of subsurface chlorophyll maximum (SCM). Further, three experiments are carried out to know the limitations in primary and secondary production in terms of nitrogen (NO3 + NH4) and silicate (Si(OH)4) in the open ocean BoB. In a “no-NO3”experiment, the nitrate limiting term [that is, NO3/(NO3 + KNO3)] is set to zero so that the difference from the control case gives the role of “regenerated production” in the total primary and secondary production. Similarly, a no-NH4 experiment was conducted to infer the role of “new production.” The new (regenerated) production fuels 85 ± 1% (28 ± 6%) of the living biomass in the East part of open ocean BoB (East BoB). The corresponding values for the west part (West BoB) are 86 ± 1% (42 ± 2%). Among the primary producers, the new (regenerated) production contributed 72 ± 1% (24 ± 6%) in the East BoB and 74 ± 1% (37 ± 2%) in the West BoB. The silicate limits the diatom production by 46% ± 22% (45% ± 27%) of the actual amount of diatom in the East BoB (West BoB) diatom. Surface to 60 m depth, we observed severe nitrate limitation over East BoB and equal limitation of nitrate and silicate over West BoB from June to September; the remaining months suffered from moderate nitrate limitation in both regions. This study shows that nitrate appears to be a limiting nutrient compared to silicate at the surface of both East and West BoB. Since silicicline is deeper than nitracline, silicate is the potential limiting nutrient in BoB from 65 to 105 m depth in all seasons.

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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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