Polarisation fluctuation in optical-fibre submarine cable under 8000 m deep sea environmental conditions

1987 ◽  
Vol 23 (3) ◽  
pp. 100 ◽  
Author(s):  
Y. Namihira ◽  
S. Ryu ◽  
K. Mochizuki ◽  
K. Furusawa ◽  
Y. Iwamoto
1987 ◽  
Vol 23 (6) ◽  
pp. 306
Author(s):  
Y. Namihira ◽  
S. Ryu ◽  
K. Mochizuki ◽  
K. Furusawa ◽  
Y. Iwamoto

1984 ◽  
Vol 20 (13) ◽  
pp. 548 ◽  
Author(s):  
Y. Ishikawa ◽  
Y. Niiro ◽  
K. Takai ◽  
H. Wakabayashi

1988 ◽  
Vol 24 (12) ◽  
pp. 749 ◽  
Author(s):  
Y. Namihira ◽  
S. Yamamoto ◽  
Y. Horiuchi ◽  
H. Wakabayashi

1988 ◽  
Vol 24 (10) ◽  
pp. 582-583 ◽  
Author(s):  
Y. Namihira ◽  
S. Ryu ◽  
H. Wakabayashi

2020 ◽  
Vol 637 ◽  
pp. 159-180
Author(s):  
ND Gallo ◽  
M Beckwith ◽  
CL Wei ◽  
LA Levin ◽  
L Kuhnz ◽  
...  

Natural gradient systems can be used to examine the vulnerability of deep-sea communities to climate change. The Gulf of California presents an ideal system for examining relationships between faunal patterns and environmental conditions of deep-sea communities because deep-sea conditions change from warm and oxygen-rich in the north to cold and severely hypoxic in the south. The Monterey Bay Aquarium Research Institute (MBARI) remotely operated vehicle (ROV) ‘Doc Ricketts’ was used to conduct seafloor video transects at depths of ~200-1400 m in the northern, central, and southern Gulf. The community composition, density, and diversity of demersal fish assemblages were compared to environmental conditions. We tested the hypothesis that climate-relevant variables (temperature, oxygen, and primary production) have more explanatory power than static variables (latitude, depth, and benthic substrate) in explaining variation in fish community structure. Temperature best explained variance in density, while oxygen best explained variance in diversity and community composition. Both density and diversity declined with decreasing oxygen, but diversity declined at a higher oxygen threshold (~7 µmol kg-1). Remarkably, high-density fish communities were observed living under suboxic conditions (<5 µmol kg-1). Using an Earth systems global climate model forced under an RCP8.5 scenario, we found that by 2081-2100, the entire Gulf of California seafloor is expected to experience a mean temperature increase of 1.08 ± 1.07°C and modest deoxygenation. The projected changes in temperature and oxygen are expected to be accompanied by reduced diversity and related changes in deep-sea demersal fish communities.


2015 ◽  
Vol 133 ◽  
pp. 176-187 ◽  
Author(s):  
Francisco J. Rodríguez-Tovar ◽  
Javier Dorador ◽  
Gloria M. Martin-Garcia ◽  
Francisco J. Sierro ◽  
José A. Flores ◽  
...  

1986 ◽  
Vol 3 (8) ◽  
pp. 373-378
Author(s):  
G. Bonaventura ◽  
F. Bigi

1986 ◽  
Vol 69 (2) ◽  
pp. 111-120 ◽  
Author(s):  
Yasuhiko Niiro ◽  
Yoshihiro Ejiri ◽  
Hitoshi Yamamoto ◽  
Yoshihiko Yamazaki ◽  
Makoto Nunokawa

Author(s):  
Jean Béguinot

In Bivalves, shell shape descriptors (in particular, elongation E, dissymmetry D, ventral convexity K) are considered functionally-relevant parameters, each of them likely being exposed to specific selective pressures, according to environmental conditions. Indeed, previous investigations, have repeatedly confirmed that different types of constraints do apply to the respective ranges of interspecific variations of E, D, K: in particular, a trend for a substantially extended range of interspecific variation of shell-elongation E (likely attributed to niche differentiation) and, on the contrary, a trend for a severely restricted range of interspecific variation of ventral-convexity K (closely centered at an optimum for mechanical resistance of valves). In turn, due to rigid geometrical relationships linking shell-shape to shell-growth, this pattern of constraints on shell-shape variations implies, mathematically, the occurrence of specifically associated covariances between shell-growth parameters, the occurrence of which were, indeed, repeatedly observed within all groups of shallow-waters clams examined so far. Yet, the fairly different environmental conditions prevailing at bathyal / abyssal depths invite addressing comparatively some typically deep-sea clams; hereafter the genus Calyptogena. Contrary to expectation, the same types of covariances between shell-growth parameters are reported in deep-sea Calyptogena as those reported in shallow-waters clams, thus suggesting less dissimilar patterns of constraints than expected between shallow waters and deep-sea conditions.


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