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干旱年份下长江口水域颗粒有机碳、氮、磷的分布特征及来源

许换林 徐文琦 牟京龙 吴念 刘素美 林贤彪

生态学杂志2025,Vol.44Issue(11):3673-3682,10.
生态学杂志2025,Vol.44Issue(11):3673-3682,10.DOI:10.13292/j.1000-4890.202511.034

干旱年份下长江口水域颗粒有机碳、氮、磷的分布特征及来源

Distributions and sources of particulate organic carbon,nitrogen,and phosphorus in the Changjiang Estu-ary during a drought year

许换林 1徐文琦 1牟京龙 1吴念 2刘素美 2林贤彪2

作者信息

  • 1. 中国海洋大学深海圈层与地球系统前沿科学中心海洋化学理论与工程技术教育部重点实验室,山东青岛 266100
  • 2. 中国海洋大学深海圈层与地球系统前沿科学中心海洋化学理论与工程技术教育部重点实验室,山东青岛 266100||青岛海洋科学与技术试点国家实验室海洋生态与环境科学功能实验室,山东青岛 266237
  • 折叠

摘要

Abstract

The year 2022 marked a period of extreme hydrological drought in the Changjiang Basin.Research on the distribution characteristics and sources of particulate biogenic elements at the Changjiang Estuary under drought plays an important role in understanding the marine biogeochemical cycles.Based on the observational data of par-ticulate organic carbon,nitrogen,and phosphorus in the Changjiang Estuary during October to November(au-tumn),we analyzed the spatial distributions of particulate organic carbon,nitrogen,and phosphorus in the estuary waters under drought season,as well as the main controlling factors.In conjunction with the particulate carbon sta-ble isotope data,a two-end-member mixing model was used to quantitatively estimate the contributions of riverine input organic matter and marine authigenic organic matter to the sources of particulate organic matter.The results showed that the concentrations of particulate organic carbon,nitrogen,and phosphorus decreased along the salinity gradient and were positively correlated with suspended particulatematter(SPM)and negatively correlated with temperature and salinity.Those results indicated that the changes of SPM in the Changjiang Estuary waters and the mixing process of salty and fresh water were important factors regulating the spatial distribution of particulate car-bon,nitrogen,and phosphorus.Areas with a significant positive deviation from the theoretical dilution line in the concentrations of particulate organic carbon,nitrogen,and phosphorus were found at the estuary and in the bottom layer of nearshore waters,corresponding to the high-value areas of SPM and chlorophyll a.This suggested that sedi-ment resuspension and biological processes played an additive role.Compared to particulate organic carbon and par-ticulate nitrogen,sediment resuspension had a stronger additive effect on particulate phosphorus,causing the ratios of carbon to nitrogen to phosphorus deviate from the Redfield ratio.The two-end-member mixing model showed that from the estuary to the nearshore and then to the offshore,the proportion of riverine input organic matter gradually decreased,while the proportion of marine authigenic organic matter gradually increased,with the proportion of ma-rine authigenic organic matter nearshore being greater than that of riverine input.Our results provided a new per-spective for understanding the response of the biogeochemical cycles in the Changjiang Estuary to extreme climate change.

关键词

长江口/颗粒有机碳、氮、磷/碳稳定同位素/空间分布/来源

Key words

Changjiang Estuary/particulate organic carbon/nitrogen and phosphorus/carbon stable isotope/spa-tial distribution/source

引用本文复制引用

许换林,徐文琦,牟京龙,吴念,刘素美,林贤彪..干旱年份下长江口水域颗粒有机碳、氮、磷的分布特征及来源[J].生态学杂志,2025,44(11):3673-3682,10.

基金项目

国家自然科学基金项目(42176040)和泰山学者项目资助. (42176040)

生态学杂志

OA北大核心

1000-4890

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