NOTE: THIS MS IS TO BE SUBMITTED FOLLOWING OUTCOME OF NATURE COMMUNICATIONS REVIEW OF A COMPANION MS. ABSTRACT (246 words, 1,457 characters including spaces) We measured the oxidation rates of N supplied as urea (UO) and ammonium (AO) in continental shelf and slope waters of the Southern Ocean west of the Antarctic Peninsula during the austral summer of 2018. The response of rates to substrate concentration varied by water mass. Rates increased moderately (up to 200%) with 440 vs 6 nM substrate amendments to samples from the Winter Water (WW, sampled at 35-100 m), but decreased (down to 7%) in samples from the Circumpolar Deep Water (CDW, 175-1000 m). AO rates decreased more than UO rates. This response suggests that CDW Thaumarchaeota are not well adapted to short-term variation in substrate concentrations and that even low amendments (we used 44 or 47 nM) may inhibit oxidation. Rates of AO and UO were not correlated; nor were they correlated with the abundance, or ratios of abundance, of marker genes; or with [NH4+]; or [urea]. UO and AO were distributed uniformly across the study area within a water mass; however, they displayed strong vertical gradients. Rates in most samples from Antarctic Surface Water (ASW, 10-15 m) were below the limit of detection. Highest rates of both processes were in samples from the WW (21.2 and 1.6 nmol L-1 d-1 for AO vs UO, respectively) and CDW (7.9 and 2.5 nmol L-1 d-1), comparable to rates from the study area reported previously. The contribution of UO to nitrite production was ~24% of that from AO alone, comparable to ratios measured at lower latitudes.
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Chemoautotrophic production In continental shelf waters off the West Antarctic Peninsula
We performed assays of chemoautotrophic carbon fixation and compared measured rates to rates predicted from oxidation of ammonia (AO), urea (UO) and nitrite (NO) N. Water samples used in this study were taken from aerobic shelf waters at stations on the continental shelf and slope west of the Antarctic Peninsula during January and February of 2018 (LMG1801). Chemoautotrophic carbon fixation rates averaged 1.8 and 1.7 nmol C L-1 d-1 in Winter Water (WW, 35-100 m) and Circumpolar Deep Water (CDW, 175-1000 m) water masses, respectively. Integrated over 1 year and a 440 m water column (excluding the Antarctic Surface Water mass, 0-34 m), chemoautotrophic production accounted for ~7 gC m2 yr-1, compared to an estimated mean annual photoautotrophic production of 180 gC m2 y-1. Chemoautotrophy in WW samples supported by AO, UO or NO was the equivalent of 0.91, 0.06, 0.13 nmol C L-1 d-1, while it was the equivalent of 0.37, 0.21 and 0.08 nmol C L-1 d-1 in samples from the CDW water mass. Chemoautotrophy coupled to AO+UO accounted for ~124% and ~55% of measured C fixation rates in these water masses, while chemoautotrophy coupled to complete nitrification (AO+UO+NO) accounted for ~128 and ~60% of measured C fixation rates. The mean turnover times for nitrite pools base on NO were 138 ± 35 d and 15 ± 3 d in WW and CDW samples, respectively. The rate of nitrite production from AO+UO in WW and CDW samples was 503 ± 233 and 24 ± 7 nmol L-1 d-1, respectively. The replacement time for the nitrite pool in the WW water mass by AO+UO calculated from these averages is 33 d while it is 9 d in the CDW. These calculations suggest the possibility of an additional sink for nitrite in the WW.
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- Award ID(s):
- 1643466
- PAR ID:
- 10468100
- Publisher / Repository:
- XIII SCAR Biology Symposium https://www.scar.org/events/biology-symposia/
- Date Published:
- Subject(s) / Keyword(s):
- ammonia-oxidation nitrite-oxidation nitrification chemoautotrophy Thaumarchaeota AOA new-production PAL-LTER Southern-Ocean
- Format(s):
- Medium: X
- Location:
- Christchurch New Zealand, 31 July 2023 to 4 August 2023
- Sponsoring Org:
- National Science Foundation
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