Referee comments for "Biological and environmental rhythms in (dark) deep-sea hydrothermal ecosystems".

2016 ◽  
Author(s):  
Anonymous
2020 ◽  
Vol 14 (8) ◽  
pp. 1994-2006 ◽  
Author(s):  
Wanpeng Wang ◽  
Zhenyu Li ◽  
Lingyu Zeng ◽  
Chunming Dong ◽  
Zongze Shao

2009 ◽  
Vol 75 (20) ◽  
pp. 6415-6421 ◽  
Author(s):  
Thomas Le Calvez ◽  
Gaëtan Burgaud ◽  
Stéphane Mahé ◽  
Georges Barbier ◽  
Philippe Vandenkoornhuyse

ABSTRACT Deep-sea hydrothermal ecosystems are considered oases of life in oceans. Since the discovery of these ecosystems in the late 1970s, many endemic species of Bacteria, Archaea, and other organisms, such as annelids and crabs, have been described. Considerable knowledge has been acquired about the diversity of (micro)organisms in these ecosystems, but the diversity of fungi has not been studied to date. These organisms are considered key organisms in terrestrial ecosystems because of their ecological functions and especially their ability to degrade organic matter. The lack of knowledge about them in the sea reflects the widely held belief that fungi are terrestrial organisms. The first inventory of such organisms in deep-sea hydrothermal environments was obtained in this study. Fungal diversity was investigated by analyzing the small-subunit rRNA gene sequences amplified by culture-independent PCR using DNA extracts from hydrothermal samples and from a culture collection that was established. Our work revealed an unsuspected diversity of species in three of the five fungal phyla. We found a new branch of Chytridiomycota forming an ancient evolutionary lineage. Many of the species identified are unknown, even at higher taxonomic levels in the Chytridiomycota, Ascomycota, and Basidiomycota. This work opens the way to new studies of the diversity, ecology, and physiology of fungi in oceans and might stimulate new prospecting for biomolecules. From an evolutionary point of view, the diversification of fungi in the oceans can no longer be ignored.


2005 ◽  
Vol 50 (3) ◽  
pp. 138-144 ◽  
Author(s):  
Anne Postec ◽  
Laurent Urios ◽  
Françoise Lesongeur ◽  
Bernard Ollivier ◽  
Joël Querellou ◽  
...  

2017 ◽  
Vol 14 (12) ◽  
pp. 2955-2977 ◽  
Author(s):  
Daphne Cuvelier ◽  
Pierre Legendre ◽  
Agathe Laës-Huon ◽  
Pierre-Marie Sarradin ◽  
Jozée Sarrazin

Abstract. During 2011, two deep-sea observatories focusing on hydrothermal vent ecology were up and running in the Atlantic (Eiffel Tower, Lucky Strike vent field) and the Northeast Pacific Ocean (NEP) (Grotto, Main Endeavour Field). Both ecological modules recorded imagery and environmental variables jointly for a time span of 23 days (7–30 October 2011) and environmental variables for up to 9 months (October 2011–June 2012). Community dynamics were assessed based on imagery analysis and rhythms in temporal variation for both fauna and environment were revealed. Tidal rhythms were found to be at play in the two settings and were most visible in temperature and tubeworm appearances (at NEP). A  ∼  6 h lag in tidal rhythm occurrence was observed between Pacific and Atlantic hydrothermal vents, which corresponds to the geographical distance and time delay between the two sites.


2016 ◽  
Author(s):  
Daphne Cuvelier ◽  
Pierre Legendre ◽  
Agathe Laes-Huon ◽  
Pierre-Marie Sarradin ◽  
Jozée Sarrazin

Abstract. During 2011, two deep-sea observatories focusing on hydrothermal vent ecology were up and running in the Atlantic (Eiffel Tower, Lucky Strike vent field) and the North-East Pacific Ocean (NEP) (Grotto, Main Endeavour field). Both ecological modules recorded imagery and environmental variables jointly for a time span of 23 days (7–30 October 2011) and environmental variables for up to 9 months (October 2011 to June 2012). Community dynamics were assessed based on imagery analysis and rhythms in temporal variation for both fauna and environment were revealed. Tidal rhythms were found to be at play in the two settings and were most visible in temperature and tubeworm appearances (at NEP). A 6-hour lag in tidal rhythm occurrence was observed between Pacific and Atlantic hydrothermal vents which corresponds to the geographical distance and time delay between the two sites.


2021 ◽  
Author(s):  
Sanglyeol Kim ◽  
Hyeongwoo Choi ◽  
Seong-il Eyun ◽  
Dongsung Kim ◽  
Ok Hwan Yu

Abstract Background: Deep-sea hydrothermal vents are dynamic environments with exotic faunas. In this study, we found a new species of Branchipolynoe (Aphroditiformia: Polynoidae) polynoid scale worm living in the recently discovered mussel Gigantidas vrijenhoeki in deep-sea hydrothermal vents and methane seeps at depths of 2,014 - 2,023 m. Associations between scale worms and giant mussels are common in hydrothermal ecosystems.Results: We analyzed the morphology of Branchipolynoe from the Onnuri vent field (OVF) on the northern Central Indian Ridge and sequenced the full mitochondrial genome. Based on its morphological traits and mitochondrial genes, we designated the specimens as Branchipolynoe onnuriensis n. sp., described herein. This species resembles B. longqiensis and B. tjiasmantoi, but is distinguished by its notopodial acicular lobe form and the tips of the subacicular neurochaetae. The identity of the new species was well supported by genetic distance and phylogenetic analyses of the mitochondrial c oxidase subunit I (COI) gene. Genetically, the new species is closest to the Western Pacific species B. tjiasmantoi; phylogenetic analyses support the correlation between Indian Ocean and Western Pacific hydrothermal polychaetes. This study provides a foundation for exploring the evolutionary relationship between scale worms and giant mussels.


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