Award: OCE-1737096

Award Title: Collaborative Research: RUI: Building a mechanistic understanding of water column chemistry alteration by kelp forests: emerging contributions of foundation species
Funding Source: NSF Division of Ocean Sciences (NSF OCE)
Program Manager: David L. Garrison

Outcomes Report

Kelp forests are among the world's most productive marine ecosystems. They are widespread in the coastal ocean, especially in temperate and sub-polar environments. Because they are so highly productive they support many other marine organisms, including fish, shellfish, and marine mammals. Their hyper-productivity also suggests that they may be able to locally reduce the impacts of ocean acidification (OA). Some coastal organisms are very sensitive to increasing seawater acidity caused by increasing levels of carbon dioxide. Shellfish larvae, in particular, are already known to be impacted by OA. We explored the possible that hyper-productivity by growing kelp may reduce this effect near to the kelp. We did so by deploying a large array of instruments that measure water column properties inside and outside of a kelp forest in Monterey Bay, California. These instruments recorded seawater circulation oxygen levels, and acidity, at minute-to-minute to day-to-day to week-to-week timescales during two summers. We saw clear differences in water chemistry between the arrays inside and outside of the kelp forest as well as between surface waters and near-bottom waters. Surface water pH was elevated inside the kelp compared to outside, suggesting that the kelp canopy locally decreased surface ocean acidification. But we observed the greatest acidification stress deeper in the water column where levels of carbon dioxide (partial pressure) reached levels as high as 1,300 μatm, about 3 times the partial pressure of carbon dioxide in air. In these acidic waters, aragonite undersaturation (ΩAr < 1) occurred on several occasions. Aragonite is an important mineral grown by developing shellfish larvae and undersaturation of the local seawater would cause stress. At this site, kelp canopy modification of seawater properties, and thus any ameliorating effect against acidification, is greatest in a narrow band of surface water, whereas the greatest acidification stress is located well below the surface canopy. The spatial disconnect between stress exposure at depth and reduction of acidification stress at the surface warrants further assessment of utilizing kelp forests as provisioners of local OA mitigation. Last Modified: 09/09/2022 Submitted by: Robert B Dunbar
DatasetLatest Version DateCurrent State
Nighttime surface chlorophyll-a concentrations at the MBARI OA1 Buoy (36° 37.373’ N, 121 ° 54.000’ W) from June to October 20182020-08-29Final no updates expected
Surface irradiance measured on the roof of the Monterey Bay Aquarium (36.62 °N, 121.90 °W) from June to October 20182020-08-29Final no updates expected
Number of new fronds recorded at the kelp forest mooring (36° 37.297’ N, 121° 54.102’ W.) at Hopkins Marine Station recorded from July to August 2018. 2020-08-29Final no updates expected
Data from moored instruments (pH, dissolved oxygen, temperature, salinity, PAR, pressure) at 9 depths outside and inside the kelp canopy at Hopkins Marine Station, recorded between June and October 2018.2020-09-02Final no updates expected
Cross-shore and alongshore velocity outside the kelp forest at Hopkins Marine Station (36° 37.342’ N, 121° 54.049’ W) recorded between June and October, 2018.2020-09-02Final no updates expected
Kelp forest mooring DIC, TA, pCO2, and aragonite saturation state estimations inside the kelp canopy (36° 37.297’ N, 121° 54.102’ W.) at Hopkins Marine Station, recorded between June and October 2018. 2020-09-02Final no updates expected
pH measured in situ over depth in the kelp forest (36° 37.3’ N, 121° 54.1’ W) recorded in July 2018.2020-10-07Final no updates expected
Dissolved Inorganic Carbon measured in situ over depth in the kelp forest (36° 37.3’ N, 121° 54.1’ W) recorded in July 2018.2020-10-07Final no updates expected
Discrete seawater samples collected at the surface, 1 m below the surface, and 1 m above the bottom two times a week at each mooring (Kelp and Outside) from June 12, 2018 to August 3, 2018.2020-10-12Final with updates expected
Cross-shore and alongshore velocity inside the kelp forest at Hopkins Marine Station (36° 37.297’ N, 121° 54.102’ W) recorded between June and October, 2018.2020-10-13Final no updates expected
CTD casts paired with bi-weekly water sampling events at instrument mooring sites near the Monterey Peninsula, California, USA from June to August 2018 and 20192021-10-19Final no updates expected
Nitrate and phosphate from various depths throughout the water column inside and outside a kelp forest near the Monterey Peninsula, California, USA from June to August 2018 and 20192021-10-20Final no updates expected
Dissolved oxygen and temperature from PME miniDOT sensors recording at 1-minute intervals at various depths on instrument moorings inside and outside of kelp forests near the Monterey Peninsula, California, USA from June to August 2018 and 20192021-11-04Final no updates expected
Water level and seafloor temperature from Onset HOBO U20L loggers deployed on the seafloor adjacent to instrument moorings inside and outside of kelp forests near the Monterey Peninsula, California, USA from June to August 2018 and 20192021-11-12Final no updates expected
Temperature data from Onset HOBO U22 loggers deployed at various depths on instrument moorings inside and outside of kelp forests near the Monterey Peninsula, California, USA from June to August 2018 and 20192021-11-15Final no updates expected
Photosynthetically active radiation (PAR) from PME miniPAR loggers deployed at the seafloor near instrument moorings inside and outside of kelp forests near the Monterey Peninsula, California, USA from June to August 2018 and 20192021-11-16Final no updates expected
Temperature data from SeaBird SBE56 sensors deployed at various depths on instrument moorings inside and outside of kelp forests near the Monterey Peninsula, California, USA from June to August 2018 and 20192021-11-17Final no updates expected

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Principal Investigator: Robert B. Dunbar (Stanford University)