ORIGINAL RESEARCH article

Front. Mar. Sci.

Sec. Marine Biogeochemistry

Volume 12 - 2025 | doi: 10.3389/fmars.2025.1612438

This article is part of the Research TopicOcean Acidification in Latin AmericaView all 3 articles

Observations of Sargassum Carbon Influx and Biogeochemical Impact in La Parguera Marine Reserve

Provisionally accepted
Priscilla N  Molina CoraPriscilla N Molina Cora1,2*Julio  Manuel MorellJulio Manuel Morell1,2*Loraine  Martell-BonetLoraine Martell-Bonet1*Luis  Raúl Rodriguez-MatosLuis Raúl Rodriguez-Matos1Julián  Emanuel MorellJulián Emanuel Morell1Maribel  Vélez-RiveraMaribel Vélez-Rivera1
  • 1Caribbean Coastal Ocean Observing System (CARICOOS), Mayaguez, Puerto Rico
  • 2University of Puerto Rico at Mayagüez, Mayagüez, Puerto Rico

The final, formatted version of the article will be published soon.

The massive influx of pelagic Sargassum spp. species, also known as Sargassum inundation events (SIEs), first arrived at the Caribbean's coastal waters in 2011. These events have been linked to hypoxia, among other ecological disturbances. Here, we report data from 2022 on (1) an assessment of the relative magnitude of particulate organic carbon (POC) load arising from SIEs into the La Parguera Marine Reserve (LPMR) basin off the southwest coast of Puerto Rico and (2) the biogeochemical impact of SIE in a nearshore mangrove key within the reserve, Monsio Jose Key Bay (MJKB). Our analysis yields that the carbon influx increased by 20% in the LPMR basin and by 103% in MJKB. Weekly observations of Sargassum input, along with the collection and analysis of water samples in MJKB, evidenced a cause-effect relation between Sargassum carbon loading and frequency of hypoxic (DO < 2 mg•L -1 ) and critically acidic conditions (Aragonite saturation, Ω < 2.0). During the 2022 Sargassum season, hypoxic conditions were detected in 43% of samples collected in MJKB. Considering the modulation of biogeochemical parameters by changes in tide height (Δh) and wind speed (m•s -1 ), stepwise multiple regression analyses (RDA-AIC model selection) showed that significant parameters influencing DO, pH, and Ω include the Sargassum carbon influx and Δh (p < 0.05). These findings strongly support the hypothesis that the additional input of POC influx enhances microbial mineralization rates responsible for depressed oxygen concentrations and acidic conditions, which could be detrimental to coastal ecosystems. This is particularly concerning in areas prone to SIEs where geomorphological features facilitate the entrainment of floating materials. Proper management requires the identification of vulnerable sites and Sargassum removal. Ongoing efforts towards that goal are underway for LPMR.

Keywords: Carbon input 1, Tropical coastal ecosystem 2, pelagic Sargassum 3, Hypoxia 4, Biogeochemistry 5, ocean acidification 6

Received: 15 Apr 2025; Accepted: 18 Jun 2025.

Copyright: © 2025 Molina Cora, Morell, Martell-Bonet, Rodriguez-Matos, Morell and Vélez-Rivera. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

* Correspondence:
Priscilla N Molina Cora, Caribbean Coastal Ocean Observing System (CARICOOS), Mayaguez, Puerto Rico
Julio Manuel Morell, Caribbean Coastal Ocean Observing System (CARICOOS), Mayaguez, Puerto Rico
Loraine Martell-Bonet, Caribbean Coastal Ocean Observing System (CARICOOS), Mayaguez, Puerto Rico

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