scholarly journals Cyanophages exhibit rhythmic infection patterns under light-dark cycles

2017 ◽  
Author(s):  
Riyue Liu ◽  
Yue Chen ◽  
Rui Zhang ◽  
Yaxin Liu ◽  
Nianzhi Jiao ◽  
...  

AbstractMost living organisms exhibit diurnal rhythms as an adaptation to the daily light-dark (diel) cycle. However, diurnal rhythms have not been found in viruses. Here, we studied the diel infection patterns of bacteriophages infecting the unicellular cyanobacteriaProchlorococcusandSynechococcus, which are the most abundant photosynthetic organisms in the oceans. With lab cultures, we found that cyanophages used three infection strategies in the dark: no adsorption, adsorption but no replication, and replication. Interestingly, the former two exhibited rhythmic infection patterns under light-dark cycles. We further showed in the South China Sea and the Western Pacific Ocean that cyanophage abundances varied rhythmically, with a peak at night. Moreover, diel transcriptional rhythms of many cyanophage genes were found in the North Pacific Subtropical Gyre, which also peaked at night. Our results suggested that cyanophage infection ofProchlorococcusis synchronized to the light-dark cycle, which may result in a synchronized release of dissolved organic matter to the marine food web.


Eos ◽  
2020 ◽  
Vol 101 ◽  
Author(s):  
Terri Cook

A comparison of primary productivity measurements across the North Pacific Ocean demonstrates the potential for using autonomous instruments to discern effects of climate change on the marine food web.



2020 ◽  
Author(s):  
Sara Ferron ◽  
Benedetto Barone ◽  
Matthew J Church ◽  
Angelicque E. White ◽  
David M. Karl


Abstract Recent evidence shows that the North Pacific subtropical gyre, the Kuroshio Extension (KE) and Oyashio Extension (OE) fronts have moved poleward in the past few decades. However, changes of the North Pacific Subtropical Fronts (STFs), anchored by the North Pacific subtropical countercurrent in the southern subtropical gyre, remain to be quantified. By synthesizing observations, reanalysis, and eddy-resolving ocean hindcasts, we show that the STFs, especially their eastern part, weakened (20%±5%) and moved poleward (1.6°±0.4°) from 1980 to 2018. Changes of the STFs are modified by mode waters to the north. We find that the central mode water (CMW) (180°-160°W) shows most significant weakening (18%±7%) and poleward shifting (2.4°±0.9°) trends, while the eastern part of the subtropical mode water (STMW) (160°E-180°) has similar but moderate changes (10% ± 8%; 0.9°±0.4°). Trends of the western part of the STMW (140°E-160°E) are not evident. The weakening and poleward shifting of mode waters and STFs are enhanced to the east and are mainly associated with changes of the northern deep mixed layers and outcrop lines—which have a growing northward shift as they elongate to the east. The eastern deep mixed layer shows the largest shallowing trend, where the subduction rate also decreases the most. The mixed layer and outcrop line changes are strongly coupled with the northward migration of the North Pacific subtropical gyre and the KE/OE jets as a result of the poleward expanded Hadley cell, indicating that the KE/OE fronts, mode waters, and STFs change as a whole system.



2013 ◽  
Vol 53 (supplement1-2) ◽  
pp. S203
Author(s):  
Mathias Girault ◽  
Hisayuki Arakawa ◽  
Gerald Gregori ◽  
Fuminori Hashihama ◽  
Hyonchol Kim ◽  
...  




2017 ◽  
Vol 8 ◽  
Author(s):  
Mary R. Gradoville ◽  
Byron C. Crump ◽  
Ricardo M. Letelier ◽  
Matthew J. Church ◽  
Angelicque E. White


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