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Abstract Recently, Gallagher et al. (2022) suggested that seaweed ecosystems are net heterotrophic carbon sources due to CO2 released from the consumption of external subsidies. Here we outline several flaws in their argument, which we believe confuse research on the blue carbon potential of seaweed ecosystems, and unjustifiably generate doubt around initiatives to protect and restore seaweed forests. Gallagher et al.’s evidence relies on 18 studies with highly variable measures of net ecosystem production, which do not statistically support their conclusion that most seaweed ecosystems are heterotrophic. This dataset is also inappropriate as it is incomplete and misrepresents seaweed ecosystems globally, particularly seaweed forests, which contribute disproportionately to global seaweed productivity. We maintain that the climate change mitigation value of an ecosystem depends on the net difference in CO2 uptake between the original ecosystem and its replacement ecosystem. We provide evidence that most seaweed ecosystems, which drawdown the largest carbon flux of any vegetated coastal habitat, are indeed net autotrophic ecosystems. We recognize that substantial uncertainties remain concerning the magnitude of CO2 drawdown by seaweed ecosystems and recommend that carbon fluxes around seaweed ecosystems should be considered more broadly and taken into account in estimates of their CO2 mitigation potential.
Hulme points out that observed rates of range expansion by invasive alien species are higher than the median speed of isotherm movement over the past 50 years, which in turn has outpaced the rates of climate-associated range changes of marine and terrestrial species ([ 1 ][1], [ 2 ][2]). This is not
Codlurn bursa, a balloon-llke chloroph~cean macroalga, a c h ~e v e s cons~derable biomass (300 g DW m-') In the NW Mediterranean httoral C bursa grows as a hollow sphere ranging in slze up to 40 cm In d~ameter, where the t h ~c k algal thallus (-0 5 cm) encloses a lumen fllled w ~t h seawater that receives substantial amounts of organlc carbon from the thallus The water enclosed within C bursa supports an active mcroheterotroph~c (bactena flagellates and clllates) community, about 2-fold denser than that in the ambient water where metazoans are absent Protlstan grazing removed the entlre bactenal populabon dally (121 7 % d-l) Oxygen concentratlon withln the enclosed water showed large die1 fluctuations, reaching concentrations close to saturat~on (-90%) dunng day time, and concentratlon close to anoxia (after 12 h) In the dark as a result of the comblned n ~e t a b o l ~s m of the alga and the microheterotrophs The relat~ve actlvlty and abundance of mlcroheterotrophs decreased as C bursa slze Increased, consistent wlth the reduct~on In the ratlo of macroalgal w e ~g h t Internal water volume That the carbon supplied by the algal enclosure becomes increasingly diluted as C bursa grows was also indicated by reduced exoproteolytic actlv~ty w t h dechne of mlcloheterotrophs abundance dunng C bursa growth The hlgh heterotroph~c actlvity w ~t h i n C bursa balloons resulted in nutnent concentrabon 5to 15-fold hlgher than those in the surround~ng seawater, w h ~c h could partially support algal production
AME Aquatic Microbial Ecology Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials AME 58:141-151 (2010) - DOI: https://doi.org/10.3354/ame01368 Temperature and phosphorus regulating carbon flux through bacteria in a coastal marine system Emma S. Kritzberg1,2,*, Jesus M. Arrieta1, Carlos M. Duarte1 1IMEDEA, CSIC-Universitat Illes Balears, Miquel Marques 21, Esporles 07190, Spain 2Lund University, Department of Ecology/Limnology, Ecology Building, 223 62 Lund, Sweden *Email: Emma.Kritzberg@limnol.lu.se ABSTRACT: The aim of this study was to explore the variation and regulation of bacterial carbon processing at a coastal oligotrophic site of the Island of Majorca in the Mediterranean Sea. In situ bacterial production (BP), respiration (BR), growth efficiency, and carbon demand in relation to environmental parameters were studied over an annual cycle. In addition, the response of bacterial carbon processing to an experimental resource (phosphate) and temperature manipulations was tested. While concentrations of dissolved organic carbon (DOC) and phosphorus were fairly stable over the year, BP and BR varied 65-fold and 79-fold, respectively. Addition of phosphate stimulated both BP and BR during most of the year, suggesting that phosphorus limitation keeps a tight rein on bacterial DOC utilization. Both BP and BR responded positively to a 2°C experimental increase, but at higher temperature increases BP and BR leveled off or decreased. In situ BP and BR were positively related to temperature, suggesting that elevated water temperature would yield increased BP and BR. BR responded more strongly to temperature than BP, suggesting that increased temperature may result in a decrease in bacterial growth efficiency. KEY WORDS: Bacterial carbon processing · Bacterial growth efficiency · Temperature regulation · Resource regulation · Phosphorus limitation Full text in pdf format PreviousNextCite this article as: Kritzberg ES, Arrieta JM, Duarte CM (2010) Temperature and phosphorus regulating carbon flux through bacteria in a coastal marine system. Aquat Microb Ecol 58:141-151. https://doi.org/10.3354/ame01368 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in AME Vol. 58, No. 2. Online publication date: January 07, 2010 Print ISSN: 0948-3055; Online ISSN: 1616-1564 Copyright © 2010 Inter-Research.
Jellyfish form spectacular blooms throughout the world's oceans. Jellyfish body plans are characterised by high water and low carbon contents which enables them to grow much larger than non-gelatinous animals of equivalent carbon content and to deviate from non-gelatinous pelagic animals when incorporated into allometric relationships. Jellyfish have, however, been argued to conform to allometric relationships when carbon content is used as the metric for comparison. Here we test the hypothesis that differences in allometric relationships for several key functional parameters remain for jellyfish even after their body sizes are scaled to their carbon content. Data on carbon and nitrogen contents, rates of respiration, excretion, growth, longevity and swimming velocity of jellyfish and other pelagic animals were assembled. Allometric relationships between each variable and the equivalent spherical diameters of jellyfish and other pelagic animals were compared before and after sizes of jellyfish were standardised for their carbon content. Before standardisation, the slopes of the allometric relationships for respiration, excretion and growth were the same for jellyfish and other pelagic taxa but the intercepts differed. After standardisation, slopes and intercepts for respiration were similar but excretion rates of jellyfish were 10× slower, and growth rates 2× faster than those of other pelagic animals. Longevity of jellyfish was independent of size. The slope of the allometric relationship of swimming velocity of jellyfish differed from that of other pelagic animals but because they are larger jellyfish operate at Reynolds numbers approximately 10× greater than those of other pelagic animals of comparable carbon content. We conclude that low carbon and high water contents alone do not explain the differences in the intercepts or slopes of the allometric relationships of jellyfish and other pelagic animals and that the evolutionary longevity of jellyfish and their propensity to form blooms is facilitated by their unique body plans.