scholarly journals The Challenge to Observe Antarctic Toothfish (Dissostichus mawsoni) Under Fast Ice

2021 ◽  
Vol 9 (3) ◽  
pp. 255
Author(s):  
Davide Di Di Blasi ◽  
Simonepietro Canese ◽  
Erica Carlig ◽  
Steven J. Parker ◽  
Eva Pisano ◽  
...  

In situ observation of Antarctic toothfish (Dissostichus mawsoni) is challenging as they typically live at depths greater than 500 m, in dark and ice-covered Antarctic waters. Searching for adequate methodologies to survey Antarctic toothfish in their habitat, we tested a miniaturized Baited Remote Underwater Video camera (BRUV), deployed through holes drilled in the sea ice in the Ross Sea region, over three field seasons. In 2015 three BRUVs were deployed at McMurdo Sound, and paired with a vertical longline sampling. In 2017, three opportunistic deployments were performed at Terra Nova Bay. In 2018 seven deployments at Terra Nova Bay provided preliminary data on the habitat preferences of the species. The design and configuration of the mini-BRUV allowed to collect high-quality video imagery of 60 Antarctic toothfish in 13 deployments from the fast sea ice. The behaviour of fish at the bait, intra-species interactions, and potential biases in individual counting were investigated, setting baselines for future studies on the abundance and distribution of Antarctic toothfish in sea-ice covered areas. This work represents the first step towards the development of protocols for non-extractive monitoring of the Antarctic toothfish in the high-Antarctica coastal shelf areas, of great value in the Ross Sea region where the largest MPA of the world has recently been established.

2021 ◽  
pp. 103510
Author(s):  
Alessandro Cau ◽  
Claudia Ennas ◽  
Davide Moccia ◽  
Olga Mangoni ◽  
Francesco Bolinesi ◽  
...  

Polar Biology ◽  
2006 ◽  
Vol 30 (6) ◽  
pp. 747-758 ◽  
Author(s):  
Letterio Guglielmo ◽  
Giacomo Zagami ◽  
Vincenzo Saggiomo ◽  
Giulio Catalano ◽  
Antonia Granata
Keyword(s):  
Sea Ice ◽  
Ross Sea ◽  

2013 ◽  
Vol 61-62 ◽  
pp. 112-124 ◽  
Author(s):  
Emanuela Rusciano ◽  
Giorgio Budillon ◽  
Giannetta Fusco ◽  
Giancarlo Spezie

2007 ◽  
Vol 19 (1) ◽  
pp. 83-92 ◽  
Author(s):  
L. Lazzara ◽  
I. Nardello ◽  
C. Ermanni ◽  
O. Mangoni ◽  
V. Saggiomo

We investigated the physical conditions of the Spring pack ice environment at Terra Nova Bay to understand their influence on the structure and physiology of sympagic microalgae. Bio-optical methods were used to study the availability and spectral quality of solar radiation, both inside and underneath the ice cover. Pack ice thickness was around 2.5 m, with a temperature between −2 and −7°C. On average, only 1.4% of surface PAR penetrated to the bottom ice and less than 0.6% below platelet ice level. Surface UV-B radiation under the bottom ice was 0.2–0.4%. Biomass concentrations up to 2400 mg Chl a m−3, dominated by two species of diatoms (Entomoneis kjellmannii and Nitschia cf. stellata), showed marked spatial and temporal patterns. Maximum values were in the platelet ice during the first half of November, and in the bottom ice two weeks later. Strong shade adaptation characteristics emerged clearly and explained the relevant abundance of microalgae within the sea ice, with specific absorption coefficients (a*) as low as 0.005 m2 (mg Chl a)−1 and the photo-acclimation index (Ek) in the range of in situ irradiance. The biomass specific production values were low, around 0.12–0.13 mg C mg Chl a−1 h−1. The hypothesis suggesting bottom ice colonization by platelet ice microalgae is supported here.


2004 ◽  
Vol 20 (sup1) ◽  
pp. 43-55 ◽  
Author(s):  
L. Guglielmo ◽  
G. C. Carrada ◽  
G. Catalano ◽  
S. Cozzi ◽  
A. Dell'Anno ◽  
...  

2001 ◽  
Vol 106 (C3) ◽  
pp. 4437-4448 ◽  
Author(s):  
Martin O. Jeffries ◽  
Kim Morris ◽  
Ted Maksym ◽  
Nickolai Kozlenko ◽  
Tina Tin

2005 ◽  
Vol 17 (2) ◽  
pp. 289-300 ◽  
Author(s):  
MARCO GROTTI ◽  
FRANCESCO SOGGIA ◽  
CARMELA IANNI ◽  
ROBERTO FRACHE

In an attempt to clarify the release of trace elements from the seasonal coastal sea ice, samples were periodically collected in a nearshore station inside the Gerlache Inlet (Terra Nova Bay, Western Ross Sea), during the summer 2000/01 and analysed for dissolved and particulate cadmium, copper, iron, manganese and lead, as well as salinity, suspended particulate matter, nutrients and phytoplankton pigments. In order to provide insight on the metal association with the particles included in the sea ice, the metal solid speciation was also investigated. Both vertical distributions within the ice cores and temporal variations at the seawater interface were studied, in an effort to fully characterize the system and correlation among the considered parameters. Concentrations and speciation patterns clearly indicate metal incorporation within the annual sea ice due to resuspension of sediments, followed by release of particulate metals during melting as a primary process affecting trace metal availability in the Antarctic coastal waters.


2008 ◽  
Vol 20 (5) ◽  
pp. 441-454 ◽  
Author(s):  
Stefano Cozzi

AbstractHigh-resolution trends of nutrients and DOM are analysed, with respect to nitrate and ammonium uptakes, in two coastal stations placed on the annual land-fast ice at Terra Nova Bay. The highest accumulations of dissolved inorganic nitrogen (87.2 µmol N dm-3), reactive phosphorus (14.1 µmol P dm-3) and reactive silicon (22.9 µmol Si dm-3) were observed in the bottom ice, although this process was preceded by a nutrient decrease in an interior sea ice layer. In the upper layer of sea ice, DOM was rather constant in concentration and P-deficient (C:N:P = 377:34:1–579:53:1). In the bottom and platelet ice, the accumulation of DOM (1277 µmol C dm-3; 108.2 µmol N dm-3; 7.67 µmol P dm-3) occurred with lower C:N:P ratios (123:14:1–59:7:1), because of a major contribution of fresher organic matter. Nitrate (< 7.33 µmol N dm-3 d-1) and ammonium (< 2.85 µmol N dm-3 d-1) uptakes in the bottom ice were higher than in the platelet ice. The comparison between the data of N-uptake and the concomitant release of total dissolved nitrogen in the bottom ice indicated that the microbial community may be subjected to low growths in situ and high releases of dissolved nitrogen, when it accumulates in this sea ice habitat.


Polar Biology ◽  
2000 ◽  
Vol 23 (2) ◽  
pp. 137-146 ◽  
Author(s):  
L. Guglielmo ◽  
G. C. Carrada ◽  
G. Catalano ◽  
A. Dell'Anno ◽  
M. Fabiano ◽  
...  

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