scholarly journals Review of "Characterizing deep-water oxygen variability and seafloor community responses using a novel autonomous lander” written by Natalya D. Gallo, Kevin Hardy, Nicholas C. Wegner, Ashley Nicoll, Haleigh Yang, and Lisa A. Levin

2020 ◽  
Author(s):  
SungHyun Nam
2020 ◽  
Author(s):  
Natalya D. Gallo ◽  
Kevin Hardy ◽  
Nicholas C. Wegner ◽  
Ashley Nicoll ◽  
Haleigh Yang ◽  
...  

Abstract. Studies on the impacts of climate change typically focus on changes to mean conditions. However, animals live in temporally variable environments which give rise to different exposure histories that could affect sensitivities to climate change. Ocean deoxygenation has been observed in nearshore, upper-slope depths in the Southern California Bight, but how these changes compared to the magnitude of natural O2 variability experienced by seafloor communities at short time-scales was unknown. We aimed to develop a low-cost and spatially flexible approach for studying nearshore, deep-sea ecosystems and monitoring deep-water oxygen variability and benthic community responses. Using a novel, autonomous hand-deployable Nanolander with an SBE MicroCAT and camera system, high-frequency environmental (O2, T, pHest) and seafloor community data were collected at depths between 100–400 m off San Diego, CA to characterize: timescales of natural environmental variability, changes in O2 variability with depth, and community responses to O2 variability. Oxygen variability was strongly linked to tidal processes, and contrary to expectation, oxygen variability did not decline linearly with depth. Depths of 200 and 400 m showed especially high O2 variability which may buffer communities at these depths to deoxygenation stress by exposing them to periods of relatively high O2 conditions across short time-scales (daily and weekly). Despite experiencing high O2 variability, seafloor communities showed limited responses to changing conditions at these shorter time-scales. Over 5-month timescales, some differences in seafloor communities may have been related to seasonal changes in the O2 regime. Overall, we found lower oxygen conditions to be associated with a transition from fish-dominated to invertebrate-dominated communities, suggesting this taxonomic shift may be a useful ecological indicator of hypoxia. Due to their small size and ease of use with small boats, hand-deployable Nanolanders can serve as a powerful capacity-building tool in data-poor regions for characterizing environmental variability and examining seafloor community sensitivity to climate-driven changes.


2020 ◽  
Author(s):  
Natalya D. Gallo ◽  
Kevin Hardy ◽  
Nicholas C. Wegner ◽  
Ashley Nicoll ◽  
Haleigh Yang ◽  
...  

2005 ◽  
Vol 50 (5) ◽  
pp. 1654-1666 ◽  
Author(s):  
Denis Gilbert ◽  
Bjorn Sundby ◽  
Charles Gobeil ◽  
Alfonso Mucci ◽  
Gilles-H. Tremblay

2012 ◽  
Vol 34 (9) ◽  
pp. 739-748 ◽  
Author(s):  
M. R. Landry ◽  
M. D. Ohman ◽  
R. Goericke ◽  
M. R. Stukel ◽  
K. A. Barbeau ◽  
...  

2012 ◽  
Vol 9 (4) ◽  
pp. 4819-4852 ◽  
Author(s):  
V. Palastanga ◽  
C. P. Slomp ◽  
C. Heinze

Abstract. The importance of particulate organic carbon and phosphorus (P) delivered from shelves on open ocean productivity, oxygen, and reactive P burial during glacial times has been assessed using a biogeochemical ocean model of the carbon (C), P and iron cycles. The model shows that in simulations of the Last Glacial Maximum (LGM) without any inputs of terrigenous material from shelves there is a moderate increase in productivity (+5 %) and mean deep water oxygen (+29 %) relative to the preindustrial simulation. However, when the input of terrigenous particulate organic C and P is considered as an additional forcing in the LGM simulation, ocean productivity increases by 46 %, mean deep water oxygen concentration decreases by 20 %, and the global rate of reactive P burial is 3 times over the preindustrial value. The associated pattern of negative oxygen anomalies at 1000 m induces a deepening of the Atlantic and Indian Ocean oxygen minimum (OMZ), while in the Pacific Ocean the OMZ is shifted to the eastern basin north of the Equator relative to preindustrial times. In addition, negative trends in oxygen extend globally below 2000 m depth, though their magnitude is rather weak, and in particular bottom waters remain above suboxic levels. Changes in dust deposition can be responsible for positive trends in reactive P burial as simulated at the LGM in open ocean regions, notably over the Southwest Atlantic and Northwest Pacific; on the other hand, inputs of terrigenous material from shelves cause an increase in P burial over the continental slope and rise regions which accounts for 47 % of the total reactive P burial change. Although the glacial-interglacial trends in P burial in our model compare well with the available observations, this study highlights the need of much more core records of C and P in open ocean settings.


2013 ◽  
Vol 6 (9) ◽  
pp. 755-760 ◽  
Author(s):  
Germain Bayon ◽  
Stéphanie Dupré ◽  
Emmanuel Ponzevera ◽  
Joël Etoubleau ◽  
Sandrine Chéron ◽  
...  

2010 ◽  
Vol 25 (4) ◽  
pp. n/a-n/a ◽  
Author(s):  
Rachel A. Mills ◽  
Sarah L. Taylor ◽  
Heiko Pälike ◽  
John Thomson

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