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Rate and fate of dissolved organic carbon release by seaweeds: A missing link in the coastal ocean carbon cycle

期刊

JOURNAL OF PHYCOLOGY
卷 57, 期 5, 页码 1375-1391

出版社

WILEY
DOI: 10.1111/jpy.13198

关键词

carbon sequestration; dissolved organic carbon; exudation; ocean carbon biogeochemical cycle; primary production; seaweeds

资金

  1. ARC [DP200101467, DP160103071]
  2. Deutsche Forschungsgemeinschaft [SCHM 3335/1-1]
  3. Australian Research Council [DP200101467] Funding Source: Australian Research Council

向作者/读者索取更多资源

The release of dissolved organic carbon (DOC) by seaweeds plays a significant role in coastal ecosystems, with factors such as seaweed species and environmental conditions influencing the rate of DOC release.
Dissolved organic carbon (DOC) release by seaweeds (marine macroalgae) is a critical component of the coastal ocean biogeochemical carbon cycle but is an aspect of seaweed carbon physiology that we know relatively little about. Seaweed-derived DOC is found throughout coastal ecosystems and supports multiple food web linkages. Here, we discuss the mechanisms of DOC release by seaweeds and group them into passive (leakage, requires no energy) and active release (exudation, requires energy) with particular focus on the photosynthetic overflow hypothesis. The release of DOC from seaweeds was first studied in the 1960s, but subsequent studies use a range of units hindering evaluation: we convert published values to a common unit (mu mol C center dot g DW-1 center dot h(-1)) allowing comparisons between seaweed phyla, functional groups, biogeographic region, and an assessment of the environmental regulation of DOC production. The range of DOC release rates by seaweeds from each phylum under ambient environmental conditions was 0-266.44 mu mol C center dot g DW-1 center dot h(-1) (Chlorophyta), 0-89.92 mu mol C center dot g DW-1 center dot h(-1) (Ochrophyta), and 0-41.28 mu mol C center dot g DW-1 center dot h(-1) (Rhodophyta). DOC release rates increased under environmental factors such as desiccation, high irradiance, non-optimal temperatures, altered salinity, and elevated dissolved carbon dioxide (CO2) concentrations. Importantly, DOC release was highest by seaweeds that were desiccated (<90 times greater DOC release compared to ambient). We discuss the impact of future ocean scenarios (ocean acidification, seawater warming, altered irradiance) on DOC release rates by seaweeds, the role of seaweed-derived DOC in carbon sequestration models, and how they inform future research directions.

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