scholarly journals Size-fractionated iron concentrations in the water column of the western North Atlantic Ocean

1994 ◽  
Vol 39 (5) ◽  
pp. 1119-1129 ◽  
Author(s):  
Jingfeng Wu ◽  
George W. Luther
2018 ◽  
Vol 15 (19) ◽  
pp. 5951-5968 ◽  
Author(s):  
Sergio Balzano ◽  
Julie Lattaud ◽  
Laura Villanueva ◽  
Sebastiaan W. Rampen ◽  
Corina P. D. Brussaard ◽  
...  

Abstract. Long chain alkyl diols (LCDs) are widespread in the marine water column and sediments, but their biological sources are mostly unknown. Here we combine lipid analyses with 18S rRNA gene amplicon sequencing on suspended particulate matter (SPM) collected in the photic zone of the western tropical North Atlantic Ocean at 24 stations to infer relationships between LCDs and potential LCD producers. The C30 1,15-diol was detected in all SPM samples and accounted for >95 % of the total LCDs, while minor proportions of C28 and C30 1,13-diols, C28 and C30 1,14-diols, as well as C32 1,15-diol were found. The concentration of the C30 and C32 diols was higher in the mixed layer of the water column compared to the deep chlorophyll maximum (DCM), whereas concentrations of C28 diols were comparable. Sequencing analyses revealed extremely low contributions (≈0.1 % of the 18S rRNA gene reads) of known LCD producers, but the contributions from two taxonomic classes with which known producers are affiliated, i.e. Dictyochophyceae and Chrysophyceae, followed a trend similar to that of the concentrations of C30 and C32 diols. Statistical analyses indicated that the abundance of 4 operational taxonomic units (OTUs) of the Chrysophyceae and Dictyochophyceae, along with 23 OTUs falling into other phylogenetic groups, were weakly (r≤0.6) but significantly (p value <0.01) correlated with C30 diol concentrations. It is not clear whether some of these OTUs might indeed correspond to C28−32 diol producers or whether these correlations are just indirect and the occurrence of C30 diols and specific OTUs in the same samples might be driven by other environmental conditions. Moreover, primer mismatches were unlikely, but cannot be excluded, and the variable number of rRNA gene copies within eukaryotes might have affected the analyses leading to LCD producers being undetected or undersampled. Furthermore, based on the average LCD content measured in cultivated LCD-producing algae, the detected concentrations of LCDs in SPM are too high to be explained by the abundances of the suspected LCD-producing OTUs. This is likely explained by the slower degradation of LCDs compared to DNA in the oxic water column and suggests that some of the LCDs found here were likely to be associated with suspended debris, while the DNA from the related LCD producers had been already fully degraded. This suggests that care should be taken in constraining biological sources of relatively stable biomarker lipids by quantitative comparisons of DNA and lipid abundances.


2021 ◽  
Author(s):  
Maribel I. García-Ibáñez ◽  
Nicholas R. Bates ◽  
Dorothee C.E. Bakker ◽  
Marcos Fontela ◽  
Antón Velo

&lt;p&gt;The uptake of carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;) from the atmosphere is changing the ocean&amp;#8217;s chemical state. Such changes, commonly known as ocean acidification, include reduction in pH and the carbonate ion concentration ([CO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;]), which in turn lowers oceanic saturation states (&amp;#937;) for calcium carbonate (CaCO&lt;sub&gt;3&lt;/sub&gt;) minerals. The &amp;#937; values for aragonite (&amp;#8486;&lt;sub&gt;aragonite&lt;/sub&gt;; one of the main CaCO&lt;sub&gt;3&lt;/sub&gt; minerals formed by marine calcifying organisms) influence the calcification rate and geographic distribution of cold-water corals (CWCs), important for biodiversity. In this work we use high-quality data of inorganic carbon measurements, collected on thirteen cruises along the same track during 1991&amp;#8211;2018, to determine the long-term trends in &amp;#8486;&lt;sub&gt;aragonite&lt;/sub&gt; in the Irminger and Iceland Basins of the North Atlantic Ocean, providing the first trends of &amp;#8486;&lt;sub&gt;aragonite&lt;/sub&gt; in the deep waters of these basins. The entire water column of both basins showed significant negative &amp;#937;&lt;sub&gt;aragonite&lt;/sub&gt; trends between -0.0015 &amp;#177; 0.0002 and -0.0061 &amp;#177; 0.0016 per year. The decrease in &amp;#937;&lt;sub&gt;aragonite&lt;/sub&gt; in the intermediate waters, where nearly half of the CWC reefs of the study region are located, caused the &amp;#937;&lt;sub&gt;aragonite&lt;/sub&gt; isolines to migrate upwards rapidly at a rate between 6 and 34 m per year. The main driver of the observed decline in &amp;#937;&lt;sub&gt;aragonite&lt;/sub&gt; in the Irminger and Iceland Basins was the increase in anthropogenic CO&lt;sub&gt;2&lt;/sub&gt;. But this was partially offset by increases in salinity (in Subpolar Mode Water), enhanced ventilation (in upper Labrador Sea Water) and increases in alkalinity (in classical Labrador Sea Water, cLSW; and overflow waters). We also found that water mass aging reinforced the &amp;#937;&lt;sub&gt;aragonite&lt;/sub&gt; decrease in cLSW. Based on the observed &amp;#937;&lt;sub&gt;aragonite&lt;/sub&gt; trends, we project that the entire water column of the Irminger and Iceland Basins will likely be undersaturated for aragonite when in equilibrium with an atmospheric mole fraction of CO&lt;sub&gt;2&lt;/sub&gt; (xCO&lt;sub&gt;2&lt;/sub&gt;) of ~860 ppmv, corresponding to climate model projections for the end of the century based on the highest CO&lt;sub&gt;2&lt;/sub&gt; emission scenarios. However, intermediate waters will likely be aragonite undersaturated when in equilibrium with an atmospheric xCO&lt;sub&gt;2&lt;/sub&gt; of ~600 ppmv, an xCO&lt;sub&gt;2&lt;/sub&gt; level slightly above that corresponding to 2 &amp;#186;C warming, thus exposing CWCs inhabiting the intermediate waters to undersaturation for aragonite.&lt;/p&gt;


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