2019
DOI: 10.1016/j.marchem.2019.103671
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Resolving the paradox: Continuous cell-free alkaline phosphatase activity despite high phosphate concentrations

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Cited by 20 publications
(18 citation statements)
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“…MEA ranged between 2.75-12.23 nmol L −1 h −1 (mean ± SE: 8.6 ± 1.5 nmol L −1 h −1 ), and DEA between 1.43-20.44 nmol L −1 h −1 (10.9 ± 4.7 nmol L −1 h −1 ). The MEA rates measured in the subantarctic waters were similar to the MEA rates measured previously in this water mass (Thomson et al, 2019) and in the North Atlantic by Steen et al (2016) but were frequently lower than some reports from the Mediterranean (Celussi and Del Negro, 2012;Celussi et al, 2019). In addition, our MEA rates were higher than those reported from the North Atlantic by (Baltar et al, 2009;Baltar et al, 2010;Baltar et al, 2013), North Pacific FIGURE 1 | Seasonal variability in temperature, phosphate, and nitrate (A), and chlorophyll-a and mean (±SE) bacterial abundance (B) in the epi-and mesopelagic layer at the study site in subantarctic waters.…”
Section: Resultssupporting
confidence: 86%
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“…MEA ranged between 2.75-12.23 nmol L −1 h −1 (mean ± SE: 8.6 ± 1.5 nmol L −1 h −1 ), and DEA between 1.43-20.44 nmol L −1 h −1 (10.9 ± 4.7 nmol L −1 h −1 ). The MEA rates measured in the subantarctic waters were similar to the MEA rates measured previously in this water mass (Thomson et al, 2019) and in the North Atlantic by Steen et al (2016) but were frequently lower than some reports from the Mediterranean (Celussi and Del Negro, 2012;Celussi et al, 2019). In addition, our MEA rates were higher than those reported from the North Atlantic by (Baltar et al, 2009;Baltar et al, 2010;Baltar et al, 2013), North Pacific FIGURE 1 | Seasonal variability in temperature, phosphate, and nitrate (A), and chlorophyll-a and mean (±SE) bacterial abundance (B) in the epi-and mesopelagic layer at the study site in subantarctic waters.…”
Section: Resultssupporting
confidence: 86%
“…A large contribution of the cell-free EEA to the total EEA has important ecological and biogeochemical implications because cell-free enzymes can be temporally and/ or spatially decoupled from the producing cell (Baltar et al, 2010;Arnosti, 2011;Baltar et al, 2016b). Since residence times for cellfree enzymes are on the scale of days to weeks (Li et al, 1998;Ziervogel et al, 2010;Arnosti, 2011;Steen and Arnosti, 2011;Baltar et al, 2013;Thomson et al, 2019), the history of the water mass may have more explanatory power than the in situ microbial community in understanding EEA dynamics (Kamer and Rassoulzadegan, 1995;Baltar et al, 2010;Arnosti 2011;Baltar et al, 2016b). It has been suggested that a high proportion of cellfree MEA might explain the paradox of "high alkaline phosphatase activity at high P i concentration" (Thomson et al, 2019).…”
Section: Introductionmentioning
confidence: 99%
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“…In many cases, Pase activity generally acts as a good indicator of the phosphorus supply for bacteria and phytoplankton (Hoppe, 2003; Luo et al, 2017). However, in some cases, Pase activities are decoupled from phosphate concentrations (Thomson et al, 2019). In comparison with the other enzymes tested in this study, Pase showed the highest activity at both 35 and 25°C (Figure 2E and Supplementary Figure S2E), the distributions of which were positively correlated with these of PO 4 3– (Pearson’s correlation test, for total EEA at 35°C, r = 0.86, p < 0.01; for dissolved EEA at 35°C, r = 0.41, p < 0.05; for total EEA at 25°C, r = 0.54, p < 0.05; for dissolved EEA at 25°C, r = 0.65, p < 0.05) (Figure 6).…”
Section: Discussionmentioning
confidence: 99%