Articles | Volume 20, issue 7
https://doi.org/10.5194/bg-20-1277-2023
© Author(s) 2023. This work is distributed under the Creative Commons Attribution 4.0 License.
Ecological divergence of a mesocosm in an eastern boundary upwelling system assessed with multi-marker environmental DNA metabarcoding
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- Final revised paper (published on 05 Apr 2023)
- Supplement to the final revised paper
- Preprint (discussion started on 10 Nov 2022)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on bg-2022-212', Anonymous Referee #1, 11 Dec 2022
- AC1: 'Reply on RC1', Markus Min, 15 Feb 2023
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RC2: 'Comment on bg-2022-212', Anonymous Referee #2, 24 Jan 2023
- AC2: 'Reply on RC2', Markus Min, 15 Feb 2023
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to minor revisions (review by editor) (15 Feb 2023) by Hans-Peter Grossart
AR by Markus Min on behalf of the Authors (02 Mar 2023)
Author's response
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ED: Publish as is (02 Mar 2023) by Hans-Peter Grossart
AR by Markus Min on behalf of the Authors (07 Mar 2023)
Min et al. performed a 50-day in situ mesocosm experiment in the Peruvian upwelling system to characterize ecological shifts in marine communities in response to upwelling events using macronutrient-rich seawater collected from an oxygen minimum zone. Their approach included using a suite of taxonomic biomarkers to capture genetic signatures across trophic levels, from bacteria to vertebrates. The initial goal seemed to be to compare simulated upwelling conditions (mesocosms) to non-upwelling conditions outside the enclosures. Instead, there was intermittent upwelling happening outside the enclosures, and the mesocosms themselves were quickly nutrient depleted and purposely stratified, characteristic of relaxed upwelling. The resulting communities in the mesocosm were dinoflagellate-dominated, which are known to dominate under stratified, low nutrient conditions.
The mesocosm experiment was an interesting exercise that seemed to evolve as the study went on. After the experiment began, the authors injected salt brine to the mesocosms to prevent vertical mixing and force stratification, added additional OMZ water, and also then added zooplankton larvae (although it’s not immediately clear why the larvae were added). More details as to why these decisions were made would be helpful for readers. After 40 days, Inca terns miraculously figured out where they could safely rest on the enclosures, made a mess and stimulated their own phytoplankton bloom(!), with their influence observed in eDNA fraction in the final days of the experiment. These factors heavily influenced the physicochemical and nutrient conditions of the mesocosm and make it a more complicated comparison that originally planned to address. The authors do a commendable job interpreting results as a function of these factors. Caution is needed in extrapolating their results to how microbial communities in this ecosystem will respond under climate-induced scenarios given these multiple variables at play. Also, temperature does not appear different between the mesocosm and Pacific samples in Fig. 2. I recommend the authors tone down this language in the abstract.
Specific Comments
Can the authors comment on why DNA samples were only taken from M1? Replication from multiple enclosures would have provided an assessment of variability and confidence in the resulting community following a period of relaxed upwelling. Did Akashiwo dominate in all other enclosures based on non-DNA evidence? I understand this information may be included in Bach et al., but would be useful to mention in this article as well for contextualization of their eDNA results.
The sequencing of blank filters was valuable and will be informative to others conducting amplicon sequencing on environmental samples. Can the authors speculate on where the diatom field-contamination came from? Gloves? Filtration rigs? Air?
Line 272 – “The MEGAN6 parameter LCA percent was from 0.80 to 0.85, depending on the marker, allowing for up to 15 – 20% of top hits to be off target and still have the majority taxonomy assigned. This parameter value was chosen to allow for minor numbers of incorrectly annotated GenBank entries – effectively allowing for ASVs which had many high quality hits to a taxa to still be assigned to that taxa even if there existed a high-bitscore hit to another GenBank sequence annotated to an unrelated taxa.”
If I am following correctly, an ASV could have been a strong match to two different organisms, and yet concretely assigned as one of them. If the query matches multiple references exceeding the annotation threshold, it would make sense for the ASV to not be annotated as either organism, and instead annotated at a broader classification level. Please explain in more detail what was done. This is particularly an issue for short rRNA amplicons – they can be 100% identical across lineages at even the order level (V9 of the 18S rRNA, for example).
How might those salinity additions have impacted cell physiology and community composition? Were there any shifts in the phytoplankton community apparent, for example with the emergence of salt-tolerant species?
Why was more OMZ water (depleted in NOx) added to mesocosms on Day 11? And why using a different mesh size than the original addition?
Line 360 – Please include a citation for referring readers to the temperature, chlorophyll and macronutrients in the other mesocosms (apart from M1).
Line 504 – Some discussion on whether amplicon sequence abundance correlates with cell biomass is needed. This is notoriously an issue for organisms with high 18S rRNA copy numbers.
Line 665 – please rephrase, sentence is not clear.