L'Atalante basin

Today, L'Atalante basin is a topic that keeps society in constant debate and reflection. From its origins to the present day, L'Atalante basin has been the object of study, admiration and controversy. Its impact on people's daily lives is undeniable, and its influence in areas such as politics, culture, technology and education is evident. Throughout history, L'Atalante basin has evolved and adapted to the needs and demands of society, becoming an indispensable element in modern life. In this article, we will explore different aspects and perspectives related to L'Atalante basin, analyzing its importance, its consequences and its future.

L'Atalante basin
L'Atalante basin is located in Mediterranean
L'Atalante basin
L'Atalante basin
Coordinates35°11′N 21°25′E / 35.18°N 21.41°E / 35.18; 21.41

L'Atalante basin is a hypersaline brine lake at the bottom of the Mediterranean Sea about 192 km (119 mi) west of the island of Crete.[1] It is named for the French L'Atalante,[2] one of the oceanographic research vessels involved in its discovery in 1993.[3] L'Atalante and its neighbors the Urania and Discovery deep hyper saline anoxic basins (DHABs) are at most 35,000 years old. They were formed by Messinian evaporite salt deposits dissolving out of the Mediterranean Ridge and collecting in abyssal depressions about 3,000 m (9,800 ft) deep.[4] L'Atalante is the smallest of the three; its surface begins at about 3,500 m (11,500 ft) below sea level.[5]

Description and biology

The L'Atalante basin's salinity is near saturation at 365 g⁄L (about 8 times that of ordinary seawater), which prevents it from mixing with the oxygenated waters above; therefore, it is completely anoxic.[5] The approximately 1.5 m (5 ft) halocline between the seawater above and brine below teems with bacterial and archaeal cells: they are chemoautotrophs, which feed on ammonia from the brine but cannot function without some oxygen. Members of archaeal anaerobic methane oxidizers group 1 (ANME-1) and haloarchaea are found only in the halocline zone. No group of organisms manages to prosper in all three zones.[5] In the brine, there are fewer cells; extremophiles predominate, including members of the deep-sea hydrothermal vent euryarchaeota (DHVEs), Methanohalophilus and Pseudomonadota (formerly Proteobacteria).[5] Eukaryotes are also found in l'Atalante, including ciliates (45%), dinoflagellates (21%) and choanoflagellates (10%).[6]

The dark gray anoxic sediments at the bottom of L'Atalante lake are covered with a 1 cm (0.4 in) loose black layer. Microbes found in the sediments are almost all (90%) various species of Bacillus.[1] In 2010, three metazoan species, all in the Loricifera phylum, were discovered living in the sediment, the first multicellular lifeforms known to live entirely without oxygen.[7][8]

References

  1. ^ a b Sass, Andrea M; McKew, Boyd A; Sass, Henrik; Fichte, Jörg; Timmis, Kenneth N; McGenity, Terry J (2008). "Diversity of Bacillus-like organisms isolated from deep-sea hyper saline anoxic sediments". Saline Systems. 4 (8). BioMed Central: 8. doi:10.1186/1746-1448-4-8. PMC 2464584. PMID 18541011.
  2. ^ "L'ATALANTE". Marinetraffic.com.
  3. ^ Aloisi, Giovanni; Castradori, Davide; Cita, Maria Bianca (2006). "Sediment injection in the pit of the Urania Anoxic brine lake (Eastern Mediterranean)". Rendiconti Lincei. 17 (3). Springer Milan: 243–262. doi:10.1007/BF02904765. S2CID 130664992.
  4. ^ Fusi, Nicoetta; de Larderel, Giovanni Aloisi; Borelu, Ada; Amelio, Ottavio; Castradori, Davide; Negri, Alessandra; Rimoldi, Bianca; Sanvoisin, Rossella; Tarbini, Paola; Cita, Maria B (1996). "Marine geology of the Medriff Corridor, Mediterranean Ridge". The Island Arc. 5 (4). The Geological Society of Japan: 420–439. Bibcode:1996IsArc...5..420F. doi:10.1111/j.1440-1738.1996.tb00163.x. Archived from the original on 2013-01-05.
  5. ^ a b c d Yakimov, Michail M; La Cono, Violetta; Denaro, Renata; D'Auria, Giuseppe; Decembrini, Franco; Timmis, Kenneth N.; Golyshin, Peter N.; Giuliano, Laura (2007). "Primary producing prokaryotic communities of brine, interface and seawater above the halo cline of deep anoxic lake L'Atalante, Eastern Mediterranean Sea". The ISME Journal. 1 (8). Nature Publishing Group: 743–755. Bibcode:2007ISMEJ...1..743Y. doi:10.1038/ismej.2007.83. PMID 18059497.
  6. ^ Alexander, Eva; Stock, Alexandra; Breiner, Hans-Werner; Behnke, Anke; Bunge, John; Yakimov, Michail M.; Stoeck, Thorsten (2009). "Microbial eukaryotes in the hypersaline anoxic L'Atalante deep-sea basin". Environmental Microbiology. 11 (2). Society for Applied Microbiology: 360–381. doi:10.1111/j.1462-2920.2008.01777.x. PMID 18826436. Archived from the original on 2013-01-05.
  7. ^ Fang, Janet (6 April 2010). "Animals thrive without oxygen at sea bottom". NatureNews.
  8. ^ Danovaro R, Dell'anno A, Pusceddu A, Gambi C, Heiner I, Kristensen RM (April 2010). "The first metazoa living in permanently anoxic conditions". BMC Biology. 8 (1): 30. doi:10.1186/1741-7007-8-30. PMC 2907586. PMID 20370908.