Effects of Mesozooplankton Growth and Reproduction on Plankton and Organic Carbon Dynamics in a Marine Biogeochemical Model

IF 5.4 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES Global Biogeochemical Cycles Pub Date : 2024-09-10 DOI:10.1029/2024GB008153
Corentin Clerc, Laurent Bopp, Fabio Benedetti, Nielja Knecht, Meike Vogt, Olivier Aumont
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Abstract

Marine mesozooplankton play an important role for marine ecosystem functioning and global biogeochemical cycles. Their size structure, varying spatially and temporally, heavily impacts biogeochemical processes and ecosystem services. Mesozooplankton exhibit size changes throughout their life cycle, affecting metabolic rates and functional traits. Despite this variability, many models oversimplify mesozooplankton as a single, unchanging size class, potentially biasing carbon flux estimates. Here, we include mesozooplankton ontogenetic growth and reproduction into a 3-dimensional global ocean biogeochemical model, PISCES-MOG, and investigate the subsequent effects on simulated mesozooplankton phenology, plankton distribution, and organic carbon export. Utilizing an ensemble of statistical predictive models calibrated with a global set of observations, we generated monthly climatologies of mesozooplankton biomass to evaluate the simulations of PISCES-MOG. Our analyses reveal that the model and observation-based biomass distributions are consistent ( r pearson ${\mathrm{r}}_{\mathit{pearson}}$  = 0.40, total epipelagic biomass: 137 TgC from observations vs. 232 TgC in the model), with similar seasonality (later bloom as latitude increases poleward). Including ontogenetic growth in the model induced cohort dynamics and variable seasonal dynamics across mesozooplankton size classes and altered the relative contribution of carbon cycling pathways. Younger and smaller mesozooplankton transitioned to microzooplankton in PISCES-MOG, resulting in a change in particle size distribution, characterized by a decrease in large particulate organic carbon (POC) and an increase in small POC generation. Consequently, carbon export from the surface was reduced by 10%. This study underscores the importance of accounting for ontogenetic growth and reproduction in models, highlighting the interconnectedness between mesozooplankton size, phenology, and their effects on marine carbon cycling.

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海洋生物地球化学模型中的中浮游生物生长和繁殖对浮游生物和有机碳动态的影响
海洋中生浮游生物在海洋生态系统功能和全球生物地球化学循环中发挥着重要作用。它们的大小结构在空间和时间上各不相同,对生物地球化学过程和生态系统服务有着重大影响。中浮游生物在整个生命周期中都会发生体型变化,从而影响新陈代谢率和功能特征。尽管存在这种变化,许多模型仍将中浮游生物过度简化为单一、不变的大小类别,从而可能导致碳通量估算出现偏差。在此,我们将中生浮游生物的本体生长和繁殖纳入三维全球海洋生物地球化学模式 PISCES-MOG,并研究其对模拟中生浮游生物物候学、浮游生物分布和有机碳输出的影响。我们利用一组经全球观测数据校准的统计预测模型,生成了中浮游生物生物量的月度气候学数据,以评估 PISCES-MOG 的模拟结果。我们的分析表明,模式和基于观测的生物量分布是一致的(r pearson ${mathrm{r}}_\mathit{pearson}}$ = 0.40,表层生物总量:观测值为 137 TgC,而模式为 232 TgC),具有相似的季节性(随着纬度向极地增加,浮游植物的开花期推迟)。将本体生长纳入模型会引起不同大小的中浮游生物的同群动态和不同的季节动态,并改变碳循环途径的相对贡献。在 PISCES-MOG 中,较年轻和较小的中浮游动物过渡到微浮游动物,导致粒径分布发生变化,其特点是大颗粒有机碳(POC)减少,小颗粒有机碳生成增加。因此,从海面输出的碳减少了 10%。这项研究强调了在模型中考虑本体生长和繁殖的重要性,突出了中浮游动物的大小、物候及其对海洋碳循环的影响之间的相互联系。
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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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