4.6 Article

Importance of internal dissolved organic nitrogen loading and cycling in a small and heavily modified coastal lagoon

期刊

BIOGEOCHEMISTRY
卷 155, 期 2, 页码 237-261

出版社

SPRINGER
DOI: 10.1007/s10533-021-00824-5

关键词

ICOLL; Allochthonous; Autochthonous; Dissolved organic matter; Organic nitrogen; Eutrophication

资金

  1. Edith Cowan University
  2. South West Catchments Council (SWCC)
  3. Department of Water and Environmental Regulation (DWER), Western Australia
  4. Geocatch, Western Australia

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Estuaries and their catchments play a crucial role in the cycling of dissolved organic matter and nutrients, with ICOLLs impacting the biogeochemical processes and release of nitrogen and carbon into coastal environments. Despite low inorganic nitrogen concentrations, the eutrophic ICOLL studied in southwest Australia experiences issues such as algal blooms and low dissolved oxygen, highlighting the importance of considering dissolved organic nitrogen in nitrogen studies. Including dissolved organic nitrogen in nitrogen studies may have a significant impact on the current understanding of the global nitrogen budget.
Estuaries are productive ecosystems that provide important ecosystem functions such as the storage and cycling of dissolved organic matter (DOM) and nutrients. Intermittently closed/open lakes and lagoons (ICOLLs) can significantly impact biogeochemical processing and release of terrestrial nitrogen and carbon into the coastal environment due to longer residence times that can extend nutrient processing within the ICOLL. Pulses of nutrient release then occur when there is connectivity between the catchment and coastal waters. It remains unclear how modifications to estuaries and their catchments impact internal processes. To better understand the balance between autochthonous and allochthonous nutrients in a heavily modified ICOLL, multiple stable isotopes (delta C-13, delta N-15) of dissolved nutrients were used to evaluate seasonal and spatial changes to nitrogen sources and sinks in a southwest Australian ICOLL. The eutrophic status of water bodies has traditionally been based on concentrations of inorganic nitrogen (DIN) (particularly NH4+ and NOx) due to its presumed higher bioavailability and association with anthropogenic pollution. However, both NH4+ and NOx concentrations were low (0 - 12.5 mu M) throughout the study area in both wet and dry seasons. Despite low surface water DIN concentrations, the system suffers from eutrophication issues such as algal blooms, low dissolved oxygen, and fish kills. The differences between the surface and porewater dissolved organic nitrogen (DON) and carbon (DOC) pools decreased in the wet season (high connectivity), suggesting that internal DOM turnover sustains eutrophication. This work demonstrates that including DON and its isotopic signature can be an effective way to study N in waterbodies with low DIN concentrations. It also highlights the need for DON, as a major constituent of total dissolved nitrogen, to be included in N studies and ultimately may have significant impact on the current understanding of the global N budget.

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