the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Influence of a small submarine canyon on biogenic matter export flux in the Lower St. Lawrence Estuary, eastern Canada
Michel Gosselin
Catherine Lalande
Alexandre Normandeau
Jean-Carlos Montero-Serrano
Khouloud Baccara
Daniel Bourgault
Owen Sherwood
Abstract. Submarine canyons enhance shelf-slope sediment exchange and influence hydrodynamic processes, with consequences for biogeochemical cycles. This work documents variations in the vertical export of biogenic matter on the northern shore of the Lower St. Lawrence Estuary (LSLE, Quebec, eastern Canada), which is characterized by the presence of an active submarine canyon system. A total of three moorings were deployed from November 2020 to September 2021. One nearshore mooring was deployed in the main axis of the Pointe-des-Monts (PDM) canyon system and was equipped with an Acoustic Doppler Current Profiler (ADCP), and two moorings equipped with sediment traps were deployed in the distal PDM canyon system and offshore Baie-Comeau (BC). The ADCP data revealed the occurrence of a minor sediment remobilization event (December 2020) and a small turbidity current (February 2021) in the canyon. Concurrent elevated fluxes of total particulate matter, particulate organic carbon, particulate nitrogen, and chloropigments showed that these events left a signature in the distal PDM sediment trap located >2.6 km further offshore. The composition of diatom and dinoflagellate assemblages was similar in the canyon system and offshore BC, but the diatom bloom occurred two weeks earlier (in mid-April) at the PDM site, where annual diatom and dinoflagellate fluxes were almost 2 times lower than at the BC site. A bloom of the potentially toxic diatom Pseudo-nitzschia seriata was also observed during the second half of September 2021 at the BC site. This study notably helps identify the relationship between near-bed canyon processes and biogenic matter export in the water column, thereby directly influencing the regional ecosystem. The study period further covered an anomalously nearly ice-free winter and thus, in the context of climate change, provides valuable insight into future trends of biogenic matter export in the LSLE.
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Hannah Sharpe et al.
Status: open (until 04 Oct 2023)
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RC1: 'Comment on egusphere-2023-1538', Kyung-Hoon Shin, 16 Sep 2023
reply
General comments: The paper investigates the impact of a submarine canyon system on the vertical export of biogenic matter in the Lower St. Lawrence Estuary, finding that sediment remobilization events and turbidity currents in the canyon influenced the flux of particulate matter and chloropigments in the water column. The study also reveals differences in diatom and dinoflagellate assemblages between the canyon system and an offshore site, with a diatom bloom occurring earlier at the canyon site. The presence of a potentially toxic diatom species was observed at the offshore site. I think this paper is a useful contribution to the literature and worthy to be published in Biogeosciences. However, I have some comments mainly about the clarity of the manuscript. I recommend the journal to accept this work after a moderate revision.
Specific comments:
Line 44: (Normandeau et al., 2014, 2020, 2022) à (Normandeau et al., 2015, 2020, 2022)
Line 329: Calvin pathway Meyers, 1994; Macdonal et al., 2004) à Calvin pathway (Meyers, 1994; Macdonal et al., 2004)
Line 347: Are there any other primary production proxies mentioned here besides chloropigments?
Table B2: symbol check! in table B2
Major comments:
- What are the conditions for determining trap depth?
- What is the reason for the decrease in water temperature and salinity in December at both sites?
- Are the large waves that occur every 2-3 years related to global ocean-atmosphere climate phenomena?
- What is the time lag for organic matter produced in the surface layer to reach the depth of the sediment trap? Can I consider that the sinking particles obtained in each month fell during that same month?
- Why does diatom bloom occur first, followed by the dinoflagellate later?
- Lines 386-390: Isn't the depth of the mixed layer greater during the fall and winter months rather than the impact of resuspension? What do you think/ or other possibility?
- Why do they exist only as cysts for Brigantedinium spp. and Selenopemphix quanta?
Citation: https://doi.org/10.5194/egusphere-2023-1538-RC1
Hannah Sharpe et al.
Hannah Sharpe et al.
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