2020
DOI: 10.1111/pre.12433
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The phenology of gross ecosystem production in a macroalga and seagrass canopy is driven by seasonal temperature

Abstract: Global changes in climatic conditions are expected to disrupt marine ecosystems. Ocean warming is one of many concerns, since more than 90% of the Earth's warming occurs in the oceans. Macrophyte-dominated communities recently have become the focus of climate mitigation due to their high carbon sequestration rate. Therefore, there is an urgent need to understand the effects of environmental variables on the phenological response of photosynthesis in entire macrophyte communities (i.e., community production). W… Show more

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Cited by 3 publications
(5 citation statements)
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“…Our study was conducted on rocky intertidal reefs at John Brown’s Beach on Japonski Island, Sitka, Alaska, USA (57.06° N, 135.37° W) 60 between September 2018 and September 2019. Measurements spanned a year to capture effects of season and temperature on ecosystem metabolism 61 . Tide pools ( n = 5, randomly selected from pools at the site) ranged from 3 to 28 L in volume, averaging 9.4 ± 4.7 L (mean ± s.e.m.…”
Section: Methodsmentioning
confidence: 99%
“…Our study was conducted on rocky intertidal reefs at John Brown’s Beach on Japonski Island, Sitka, Alaska, USA (57.06° N, 135.37° W) 60 between September 2018 and September 2019. Measurements spanned a year to capture effects of season and temperature on ecosystem metabolism 61 . Tide pools ( n = 5, randomly selected from pools at the site) ranged from 3 to 28 L in volume, averaging 9.4 ± 4.7 L (mean ± s.e.m.…”
Section: Methodsmentioning
confidence: 99%
“…Reliable long-term field observations of carbon capture rates by macroalgae ecosystems remains scarce. Presently, most assessments of carbon capture rates rely on extrapolating from chambered photosynthesis experiments of using phytoelements or the whole thallus of macroalgae, measuring the CO 2 flux at the airsea interface and the O 2 flux at the water-sediment interface using eddy covariance techniques (e.g., Berg et al, 2022), extrapolate from simulations and limited in temporal scope (e.g., Watanabe et al, 2020), extrapolate from O 2 mass-balances (e.g., Hinode et al, 2020), measuring the O 2 flux at the water-sediment, and isotopic measurements (e.g., Holtgrieve et al, 2010;Staehr et al, 2012;Hoellein et al, 2013). All methods have both advantages and disadvantages, that must be considered prior to data interpretation.…”
Section: Discussionmentioning
confidence: 99%
“…The instruments were placed so that the majority of the biomass of the seaweed were between the data loggers. Recordings were carried out for four to twenty days before the instruments were retrieved for maintenance and data offloading (e.g., Hinode et al, 2020). Calculations of productivity (as described below) is based on the ensemble mean of the dissolved oxygen time-series recorded by the dataloggers, to account for vertical heterogeneity.…”
Section: Temperature and Dissolved Oxygenmentioning
confidence: 99%
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