Spatio-temporal distribution and abundance of Euphausia crystallorophias in Terra Nova Bay (Ross Sea, Antarctica) during austral summer

Polar Biology ◽  
2008 ◽  
Vol 32 (3) ◽  
pp. 347-367 ◽  
Author(s):  
Letterio Guglielmo ◽  
P. Donato ◽  
G. Zagami ◽  
A. Granata
2020 ◽  
Vol 8 (9) ◽  
pp. 1273
Author(s):  
Renata Zaccone ◽  
Cristina Misic ◽  
Filippo Azzaro ◽  
Maurizio Azzaro ◽  
Giovanna Maimone ◽  
...  

The active prokaryotic communities proliferate in the ecosystems of the Antarctic Ocean, participating in biogeochemical cycles and supporting higher trophic levels. They are regulated by several environmental and ecological forcing, such as the characteristics of the water masses subjected to global warming and particulate organic matter (POM). During summer 2017, two polynyas in the Ross Sea were studied to evaluate key-microbiological parameters (the proteasic, glucosidasic, and phosphatasic activities, the microbial respiratory rates, the prokaryotic abundance and biomass) in relation to quantitative and qualitative characteristics of POM. Results showed significant differences in the epipelagic layer between two macro-areas (Terra Nova Bay and Ross Sea offshore area). Proteins and carbohydrates were metabolized rapidly in the offshore area (as shown by turnover times), due to high enzymatic activities in this zone, indicating fresh and labile organic compounds. The lower quality of POM in Terra Nova Bay, as shown by the higher refractory fraction, led to an increase in the turnover times of proteins and carbohydrates. Salinity was the physical constraint that played a major role in the distribution of POM and microbial activities in both areas.


Polar Biology ◽  
1995 ◽  
Vol 15 (7) ◽  
Author(s):  
Carlo Andreoli ◽  
Claudio Tolomio ◽  
Isabella Moro ◽  
Marco Radice ◽  
Emanuela Moschin ◽  
...  

2019 ◽  
Author(s):  
Seung-Tae Yoon ◽  
Won Sang Lee ◽  
Craig Stevens ◽  
Stefan Jendersie ◽  
SungHyun Nam ◽  
...  

Abstract. The formation of High-Salinity Shelf Water (HSSW), which is the major source of Antarctic bottom water (AABW), has been observed in Terra Nova Bay (TNB) in Antarctica. We believe a description of the spatio-temporal variation of salinity in TNB would help understand the production of HSSW in the region. Hence, the aim of this study is to investigate salinity variations in the Drygalski Basin (DB) and eastern TNB close to Crary Bank of the Ross Sea. For this, we use the moored and profiled hydrographic data, as well as available wind and sea-ice products. We found that deep-ocean salinity in the eastern TNB (~ 660 m) and DB (~ 1200 m) increases each year starting in September, and large amounts of salinity increase (> 0.04) were observed in 2016 and 2017. According to the velocity data observed at the same depths, the increases in salinity from September were due to the advection of HSSW from the coastal region of the Nansen ice shelf (NIS). The significant increases in salinity are related to the formation of active HSSW, evidence of which can be found from the HSSW properties obtained in February 2017 and March 2018. In addition, we show that HSSW can locally formed in the upper layer (


2002 ◽  
Vol 36 (1-2) ◽  
pp. 29-49 ◽  
Author(s):  
S. Fonda Umani ◽  
A. Accornero ◽  
G. Budillon ◽  
M. Capello ◽  
S. Tucci ◽  
...  

Chemosphere ◽  
2017 ◽  
Vol 185 ◽  
pp. 1122-1135 ◽  
Author(s):  
S. Illuminati ◽  
A. Annibaldi ◽  
T. Romagnoli ◽  
G. Libani ◽  
M. Antonucci ◽  
...  

1998 ◽  
Vol 17 (1-4) ◽  
pp. 425-434 ◽  
Author(s):  
G. Albertelli ◽  
R. Cattaneo-Vietti ◽  
M. Chiantore ◽  
A. Pusceddu ◽  
M. Fabiano

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

2011 ◽  
Vol 52 (57) ◽  
pp. 291-300 ◽  
Author(s):  
Stefan Kern ◽  
Stefano Aliani

AbstractWintertime (April–September) area estimates of the Terra Nova Bay polynya (TNBP), Antarctica, based on satellite microwave radiometry are compared with in situ observations of water salinity, temperature and currents at a mooring in Terra Nova Bay in 1996 and 1997. In 1996, polynya area anomalies and associated anomalies in polynya ice production are significantly correlated with salinity anomalies at the mooring. Salinity anomalies lag area and/or ice production anomalies by about 3 days. Up to 50% of the variability in the salinity at the mooring position can be explained by area and/or ice production anomalies in the TNBP for April–September 1996. This value increases to about 70% when considering shorter periods like April–June or May–July, but reduces to 30% later, for example July–September, together with a slight increase in time lag. In 1997, correlations are smaller, less significant and occur at a different time lag. Analysis of ocean currents at the mooring suggests that in 1996 conditions were more favourable than in 1997 for observing the impact of descending plumes of salt-enriched water formed in the polynya during ice formation on the water masses at the mooring depth.


2004 ◽  
Vol 23 (2) ◽  
pp. 141-146 ◽  
Author(s):  
Maria De Domenico ◽  
Angelina Lo Giudice ◽  
Luigi Michaud ◽  
Marcello Saitta ◽  
Vivia Bruni

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