scholarly journals Unexpected diversity of Endozoicomonas in deep-sea corals

Author(s):  
CA Kellogg ◽  
ZA Pratte
Keyword(s):  
Deep Sea ◽  
2004 ◽  
Vol 219 (3-4) ◽  
pp. 297-309 ◽  
Author(s):  
Norbert Frank ◽  
Martine Paterne ◽  
Linda Ayliffe ◽  
Tjeerd van Weering ◽  
Jean-Pierre Henriet ◽  
...  

2020 ◽  
Author(s):  
◽  
Moses Thiong'o

The oceans make up about 70% of the earth’s surface and serve as habitats for many deep and shallow creatures. In depths of about 50 meters and more, deep-sea corals and sponges occur mostly along seamounts, continental margins, undersea canyons and ridges. They, deep-sea corals and sponges, play a key role in supporting the health of the ocean as they preserve the biodiversity and long-term sustainability of commercial and recreational fish species. With the many benefits that are attached to deep-sea corals and sponges, the Deep-Sea Corals and Research Technology Program (DSCRTP) has been collecting coral and sponge location data from hundreds of remotely operated vehicle (ROV) surveys. However, DSCRTP does not have a spatial representation of the area covered by each ROV while searching for corals and sponges in the deep-sea. A spatial representation would provide critical information to researchers and managers to understand where a survey for corals and sponges has happened, and where a survey is yet to be done in the deep-sea. Therefore, the goal of this study is to create a spatial representation of the ROV surveys that have been collected in Monterey Bay and Hawaii sections of the deep-sea.


2011 ◽  
Vol 75 (16) ◽  
pp. 4416-4425 ◽  
Author(s):  
Nivedita Thiagarajan ◽  
Jess Adkins ◽  
John Eiler

Author(s):  
Andrew P. DeVogelaere ◽  
Erica J. Burton ◽  
Tonatiuh Trejo ◽  
Chad E. King ◽  
David A. Clague ◽  
...  

Radiocarbon ◽  
1989 ◽  
Vol 31 (03) ◽  
pp. 533-543 ◽  
Author(s):  
Sheila Griffin ◽  
Ellen R M Druffel

Radiocarbon measurements in deep-sea corals from the Little Bahama Bank were used to determine the source of carbon to the skeletal matrices. Specimens of Lophelia, Gerardia, Paragorgia johnsoni and Corallium noibe were sectioned according to visible growth rings and/or stem diameter. We determined that the source of carbon to the corals accreting organic matter was primarily from surface-derived sources. Those corals that accrete a calcerous skeleton were found to obtain their carbon solely from dissolved inorganic carbon (DIC) in sea water from the depth at which the corals grew. These results, in conjunction with growth-rate studies using short-lived radioisotopes, support the use of deep-sea corals to reconstruct time histories of transient and non-transient tracers at depth in the oceans.


2016 ◽  
Vol 129 ◽  
pp. 196-212 ◽  
Author(s):  
Nancy G. Prouty ◽  
Charles R. Fisher ◽  
Amanda W.J. Demopoulos ◽  
Ellen R.M. Druffel

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