90Sr and137Cs contents in the surface waters of the adjacent seas of Japan and the North Pacific during 1969 to 1973

1976 ◽  
Vol 32 (5) ◽  
pp. 228-234 ◽  
Author(s):  
Yutaka Nagaya ◽  
Kiyoshi Nakamura
Radiocarbon ◽  
2001 ◽  
Vol 43 (1) ◽  
pp. 15-25 ◽  
Author(s):  
Ellen R M Druffel ◽  
S Griffin ◽  
T P Guilderson ◽  
M Kashgarian ◽  
J Southon ◽  
...  

We show that high-precision radiocarbon (Δ14C) measurements from annual bands of a Hawaiian surface coral decreased by 7‰ from AD 1893 to 1952. This decrease is coincident with the Suess Effect, which is mostly due to the dilution of natural levels of 14C by 14C-free fossil fuel CO2. This decrease is equal to that expected in surface waters of the subtropical gyres, and indicates that the surface waters of the North Pacific were in steady state with respect to long term mixing of CO2 during the past century. Correlation between Δ14C and North Pacific gyre sea surface temperatures indicates that vertical mixing local to Hawaii and the North Pacific gyre as a whole is the likely physical mechanism to result in variable Δ14C. Prior to 1920, this correlation starts to break down; this may be related to the non-correlation between biennial Δ14C values in corals from the southwest Pacific and El Niño events observed during this period as well.


2011 ◽  
Vol 45 (23) ◽  
pp. 9874-9882 ◽  
Author(s):  
Céline Gallon ◽  
Mara A. Ranville ◽  
Christopher H. Conaway ◽  
William M. Landing ◽  
Clifton S. Buck ◽  
...  

Nature ◽  
2010 ◽  
Vol 465 (7301) ◽  
pp. 1062-1065 ◽  
Author(s):  
Kenneth S. Johnson ◽  
Stephen C. Riser ◽  
David M. Karl

1965 ◽  
Vol 22 (3) ◽  
pp. 841-847 ◽  
Author(s):  
R. Ward Renshaw

The medusa, Calycopsis nematophora, is reported from the North Pacific for the first time since its original description. It is restricted to arctic-subarctic surface waters. Radial canal variation and other morphological characters are discussed.


2015 ◽  
Vol 10 (6) ◽  
pp. 1308-1322 ◽  
Author(s):  
Jessica A Bryant ◽  
Frank O Aylward ◽  
John M Eppley ◽  
David M Karl ◽  
Matthew J Church ◽  
...  

2021 ◽  
Vol 12 ◽  
Author(s):  
Fuyan Li ◽  
Andy Leu ◽  
Kirsten Poff ◽  
Laura T. Carlson ◽  
Anitra E. Ingalls ◽  
...  

Thaumarchaeota and Thermoplasmatota are the most abundant planktonic archaea in the sea. Thaumarchaeota contain tetraether lipids as their major membrane lipids, but the lipid composition of uncultured planktonic Thermoplasmatota representatives remains unknown. To address this knowledge gap, we quantified archaeal cells and ether lipids in open ocean depth profiles (0–200 m) of the North Pacific Subtropical Gyre. Planktonic archaeal community structure and ether lipid composition in the water column partitioned into two separate clusters: one above the deep chlorophyll maximum, the other within and below it. In surface waters, Thermoplasmatota densities ranged from 2.11 × 106 to 6.02 × 106 cells/L, while Thaumarchaeota were undetectable. As previously reported for Thaumarchaeota, potential homologs of archaeal tetraether ring synthases were present in planktonic Thermoplasmatota metagenomes. Despite the absence of Thaumarchaeota in surface waters, measurable amounts of intact polar ether lipids were found there. Based on cell abundance estimates, these surface water archaeal ether lipids contributed only 1.21 × 10–9 ng lipid/Thermoplasmatota cell, about three orders of magnitude less than that reported for Thaumarchaeota cells. While these data indicate that even if some tetraether and diether lipids may be derived from Thermoplasmatota, they would only comprise a small fraction of Thermoplasmatota total biomass. Therefore, while both MGI Thaumarchaeota and MGII/III Thermoplasmatota are potential biological sources of archaeal GDGTs, the Thaumarchaeota appear to be the major contributors of archaeal tetraether lipids in planktonic marine habitats. These results extend and confirm previous reports of planktonic archaeal lipid sources, and further emphasize the need for Thermoplasmatota cultivation, to better characterize the membrane lipid constituents of marine planktonic Thermoplasmatota, and more precisely define the sources and patterns of archaeal tetraether lipid distributions in marine plankton.


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