Abstract:Seagrass ecosystems are expected to benefit from the global increase in CO2 in the ocean because the photosynthetic rate of these plants may be Ci-limited at the current CO2 level. As well, it is expected that lower external pH will facilitate the nitrate uptake of seagrasses if nitrate is cotransported with H+ across the membrane as in terrestrial plants. Here, we investigate the effects of CO2 enrichment on both carbon and nitrogen metabolism of the seagrass Zostera noltii in a mesocosm experiment where plan… Show more
“…The short-term gas exchange measurements with CO 2 enrichment conditions clearly indicated that Z. noltei community production at around the same irradiance level increased 1.5-fold. Higher community production under CO 2 enrichment suggest that community production of Z. noltei are carbon limited under the current atmospheric CO 2 concentration, confirming the same conclusions previously obtained for Z. noltei (Alexandre et al, 2012) and for Z. marina (Beer and Koch, 1996;Zimmerman et al, 1997;Invers et al, 2001). These reports are on the photosynthetic response of individual plants rather than whole community, but it is expected that the increase in photosynthetic rate of individual plants is reflected on the higher organizational level of the community production.…”
Section: Co 2 Enrichmentsupporting
confidence: 87%
“…This was also observed in Z. marina (Zimmerman et al, 1997 and Z. noltei (Alexandre et al, 2012) where increase in CO 2 concentrations increased the light using capacity of individual plants.…”
Section: Par Responsessupporting
confidence: 61%
“…Most of the studies on the effects of elevated CO 2 levels on seagrasses have been on the responses of productivity and light requirements (Beer and Koch, 1996;Thom, 1996;Zimmerman et al, 1997;Palacios and Zimmerman, 2007), photosynthetic and leaf growth rates (Alexandre et al, 2012) and the uptake rate of ammonium and nitrate (Short and Neckles, 1999;Alexandre et al, 2012;Ow et al, 2016). Results so far have suggested that, seagrass meadows can utilize the increased CO 2 concentration from the water column and enhance their photosynthetic activity and community metabolism (Frankignoulle and Disteche, 1984;Frankignoulle and Bouquegneau, 1990;Invers et al, 2001).…”
In situ production responses of air-exposed intertidal communities under CO 2 enrichment are reported here for the first time. We assessed the short-term effects of CO 2 on the light responses of the net community production (NCP) and community respiration (CR) of intertidal Z. noltei and unvegetated sediment communities of Ria Formosa lagoon, when exposed to air. NCP and CR were measured in situ in summer and winter, under present and CO 2 enriched conditions using benthic chambers. Within chamber CO 2 evolution measurements were carried out by a series of short-term incubations (30 min) using an infra-red gas analyser. Liner regression models fitted to the NCP-irradiance responses were used to estimate the seasonal budgets of air-exposed, intertidal production as determined by the daily and seasonal variation of incident photosynthetic active radiation. High CO 2 resulted in higher CO 2 sequestration by both communities in both summer and winter seasons. Lower respiration rates of both communities under high CO 2 further contributed to a potential negative climate feedback, except in winter when the CR of sediment community was higher. The light compensation points (LCP) (light intensity where production equals respiration) of Z. noltei and sediment communities also decreased under CO 2 enriched conditions in both seasons. The seasonal community production of Z. noltei was 115.54 ± 7.58 g C m −2 season −1 in summer and 29.45 ± 4.04 g C m −2 season −1 in winter and of unvegetated sediment was 91.28 ± 6.32 g C m −2 season −1 in summer and 25.83 ± 4.01 g C m −2 season −1 in winter under CO 2 enriched conditions. Future CO 2 conditions may increase air-exposed seagrass production by about 1.5-fold and unvegetated sediments by about 1.2-fold.
“…The short-term gas exchange measurements with CO 2 enrichment conditions clearly indicated that Z. noltei community production at around the same irradiance level increased 1.5-fold. Higher community production under CO 2 enrichment suggest that community production of Z. noltei are carbon limited under the current atmospheric CO 2 concentration, confirming the same conclusions previously obtained for Z. noltei (Alexandre et al, 2012) and for Z. marina (Beer and Koch, 1996;Zimmerman et al, 1997;Invers et al, 2001). These reports are on the photosynthetic response of individual plants rather than whole community, but it is expected that the increase in photosynthetic rate of individual plants is reflected on the higher organizational level of the community production.…”
Section: Co 2 Enrichmentsupporting
confidence: 87%
“…This was also observed in Z. marina (Zimmerman et al, 1997 and Z. noltei (Alexandre et al, 2012) where increase in CO 2 concentrations increased the light using capacity of individual plants.…”
Section: Par Responsessupporting
confidence: 61%
“…Most of the studies on the effects of elevated CO 2 levels on seagrasses have been on the responses of productivity and light requirements (Beer and Koch, 1996;Thom, 1996;Zimmerman et al, 1997;Palacios and Zimmerman, 2007), photosynthetic and leaf growth rates (Alexandre et al, 2012) and the uptake rate of ammonium and nitrate (Short and Neckles, 1999;Alexandre et al, 2012;Ow et al, 2016). Results so far have suggested that, seagrass meadows can utilize the increased CO 2 concentration from the water column and enhance their photosynthetic activity and community metabolism (Frankignoulle and Disteche, 1984;Frankignoulle and Bouquegneau, 1990;Invers et al, 2001).…”
In situ production responses of air-exposed intertidal communities under CO 2 enrichment are reported here for the first time. We assessed the short-term effects of CO 2 on the light responses of the net community production (NCP) and community respiration (CR) of intertidal Z. noltei and unvegetated sediment communities of Ria Formosa lagoon, when exposed to air. NCP and CR were measured in situ in summer and winter, under present and CO 2 enriched conditions using benthic chambers. Within chamber CO 2 evolution measurements were carried out by a series of short-term incubations (30 min) using an infra-red gas analyser. Liner regression models fitted to the NCP-irradiance responses were used to estimate the seasonal budgets of air-exposed, intertidal production as determined by the daily and seasonal variation of incident photosynthetic active radiation. High CO 2 resulted in higher CO 2 sequestration by both communities in both summer and winter seasons. Lower respiration rates of both communities under high CO 2 further contributed to a potential negative climate feedback, except in winter when the CR of sediment community was higher. The light compensation points (LCP) (light intensity where production equals respiration) of Z. noltei and sediment communities also decreased under CO 2 enriched conditions in both seasons. The seasonal community production of Z. noltei was 115.54 ± 7.58 g C m −2 season −1 in summer and 29.45 ± 4.04 g C m −2 season −1 in winter and of unvegetated sediment was 91.28 ± 6.32 g C m −2 season −1 in summer and 25.83 ± 4.01 g C m −2 season −1 in winter under CO 2 enriched conditions. Future CO 2 conditions may increase air-exposed seagrass production by about 1.5-fold and unvegetated sediments by about 1.2-fold.
“…On the other hand, in a long-term experiment, there was no effect of increasing CO 2 levels on the aboveground productivity of Zostera marina (Palacios and Zimmerman, 2007), as opposed to belowground. Alexandre et al (2012) showed that the net photosynthetic rate of Zostera noltii was positively affected by the CO 2 enrichment of the seawater, but they did not observe an increase in leaf growth rates.…”
Section: Lauritano Et Al: Response Of Key Stress-related Genes Ofmentioning
Abstract. Submarine volcanic vents are being used as natural laboratories to assess the effects of increased ocean acidity and carbon dioxide (CO 2 ) concentration on marine organisms and communities. However, in the vicinity of volcanic vents other factors in addition to CO 2 , which is the main gaseous component of the emissions, may directly or indirectly confound the biota responses to high CO 2 . Here we used for the first time the expression of antioxidant and stress-related genes of the seagrass Posidonia oceanica to assess the stress levels of the species. Our hypothesis is that unknown factors are causing metabolic stress that may confound the putative effects attributed to CO 2 enrichment only. We analyzed the expression of 35 antioxidant and stressrelated genes of P. oceanica in the vicinity of submerged volcanic vents located in the islands of Ischia and Panarea, Italy, and compared them with those from control sites away from the influence of vents. Reverse-transcription quantitative polymerase chain reaction (RT-qPCR) was used to characterize gene expression patterns.Fifty-one percent of genes analyzed showed significant expression changes. Metal detoxification genes were mostly down-regulated in relation to controls at both Ischia and Panarea, indicating that P. oceanica does not increase the synthesis of heavy metal detoxification proteins in response to the environmental conditions present at the two vents. The up-regulation of genes involved in the free radical detoxification response (e.g., CAPX, SODCP and GR) indicates that, in contrast with Ischia, P. oceanica at the Panarea site faces stressors that result in the production of reactive oxygen species, triggering antioxidant responses. In addition, heat shock proteins were also activated at Panarea and not at Ischia. These proteins are activated to adjust stressaccumulated misfolded proteins and prevent their aggregation as a response to some stressors, not necessarily high temperature. This is the first study analyzing the expression of target genes in marine plants living near natural CO 2 vents. Our results call for contention to the general claim of seagrasses as "winners" in a high-CO 2 world, based on observations near volcanic vents. Careful consideration of factors that are at play in natural vents sites other than CO 2 and acidification is required. This study also constitutes a first step for using stress-related genes as indicators of environmental pressures in a changing ocean.
“…Under such conditions, photosynthetic carbon assimilation is increased and photorespiration, which can reduce photosynthetic capacity of eelgrass by 40%, is decreased (e.g., Thom 1995;Zimmerman et al 1997;Palacios and Zimmerman 2007;Alexandre et al 2012;Buapet et al 2013). The most convincing evidence has been provided by Zimmerman and coworkers who have simulated coastal acidification in manipulative experiments with eelgrass for nearly two decades.…”
Introduction: The Chesapeake Bay was once renowned for expansive meadows of submerged aquatic vegetation (SAV). However, only 10% of the original meadows survive. Future restoration efforts will be complicated by accelerating climate change, including physiological stressors such as a predicted mean temperature increase of 2-6°C and a 50-160% increase in CO 2 concentrations. Outcomes: As the Chesapeake Bay begins to exhibit characteristics of a subtropical estuary, summer heat waves will become more frequent and severe. Warming alone would eventually eliminate eelgrass (Zostera marina) from the region. It will favor native heat-tolerant species such as widgeon grass (Ruppia maritima) while facilitating colonization by non-native seagrasses (e.g., Halodule spp.). Intensifying human activity will also fuel coastal zone acidification and the resulting high CO 2 /low pH conditions may benefit SAV via a "CO 2 fertilization effect." Discussion: Acidification is known to offset the effects of thermal stress and may have similar effects in estuaries, assuming water clarity is sufficient to support CO 2 -stimulated photosynthesis and plants are not overgrown by epiphytes. However, coastal zone acidification is variable, driven mostly by local biological processes that may or may not always counterbalance the effects of regional warming. This precarious equipoise between two forcesthermal stress and acidification -will be critically important because it may ultimately determine the fate of cool-water plants such as Zostera marina in the Chesapeake Bay. Conclusion: The combined impacts of warming, coastal zone acidification, water clarity, and overgrowth of competing algae will determine the fate of SAV communities in rapidly changing temperate estuaries.
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