scholarly journals Inefficient microbial production of refractory dissolved organic matter in the ocean

2015 ◽  
Vol 6 (1) ◽  
Author(s):  
Helena Osterholz ◽  
Jutta Niggemann ◽  
Helge-Ansgar Giebel ◽  
Meinhard Simon ◽  
Thorsten Dittmar
Keyword(s):  
Organic Matter ◽  
Dissolved Organic Matter ◽  
Microbial Production

Systematic microbial production of optically active dissolved organic matter in subarctic lake water

2019 ◽  
Vol 65 (5) ◽  
pp. 951-961
Author(s):  
Martin Berggren ◽  
Cristian Gudasz ◽  
Francois Guillemette ◽  
Geert Hensgens ◽  
Linlin Ye ◽  
...  
Keyword(s):  
Organic Matter ◽  
Dissolved Organic Matter ◽  
Lake Water ◽  
Optically Active ◽  
Microbial Production ◽  
Subarctic Lake

Organic matter content controls the N and P degradation process on biogeochemical interfaces: A micro-ecosystem scale study based on SoilChips-XPS-Zymography integrated technique in paddy soils

2020 ◽  
Author(s):  
Liang Wei
Keyword(s):  
Organic Matter ◽  
Dissolved Organic Matter ◽  
Photoelectron Spectroscopy ◽  
Organic Matter Content ◽  
Degradation Process ◽  
Matter Content ◽  
Microbial Production ◽  
Paddy Soils ◽  
Rrna Gene ◽  
Degradation Processes

<p>The biogeochemical interfaces are hotspots for organic matter (OM) transformation. However, direct and continuouxiacis tracing of OM transformations and N and P degradation processes are lacking due to the heterogeneous and opaque nature of soil microenvironment. To investigate these processes, a new soil microarray technology (SoilChips) was developed and used. Homogeneous 2-mm-diameter SoilChips were constructed by depositing a dispersed paddy soils with high and low soil organic carbon (SOC) content. A horizon suspension on a patterned glass. Dissolved organic matter from the original soil was added on the SoilChips to mimic biogeochemical processes on interfaces. The chemical composition of biogeochemical interfaces were evaluated via X-ray photoelectron spectroscopy (XPS) and the two-dimensional distribution of enzyme activities in SoilChips were evaluated by zymography. Over 30 days, soil with high SOC content increases microbial nutrition (N and P) requirements than soil with low SOC evidenced by higher hotspots of β-1,4-N-acetaminophen glucosidase, and acid phosphomonoesterases and higher 16S rRNA gene copies. The degree of humification in dissolved organic matter (DOM) was higher and the bioavailability of DOM was poorer in soil with high SOC than soil with low SOC. The poorest bioavailability of DOM was detected at the end of incubation in soil with high SOC. Molecular modeling of OM composition showed that low SOC mainly facilitated the microbial production of glucans but high SOC mainly facilitated the microbial production of proteins. We demonstrated that SOC content or DOM availability for microorganisms modifies the specific OM molecular processing and N and P degradation processes, thereby providing a direct insight into biogeochemical transformation of OM at micro-scale.</p>

Microbial production of recalcitrant dissolved organic matter: long-term carbon storage in the global ocean

2010 ◽  
Vol 8 (8) ◽  
pp. 593-599 ◽  
Author(s):  
Nianzhi Jiao ◽  
Gerhard J. Herndl ◽  
Dennis A. Hansell ◽  
Ronald Benner ◽  
Gerhard Kattner ◽  
...  
Keyword(s):  
Organic Matter ◽  
Dissolved Organic Matter ◽  
Carbon Storage ◽  
Microbial Production ◽  
Global Ocean

scholarly journals Tracing the long-term microbial production of recalcitrant fluorescent dissolved organic matter in seawater

2014 ◽  
Vol 41 (7) ◽  
pp. 2481-2488 ◽  
Author(s):  
Linda Jørgensen ◽  
Colin A. Stedmon ◽  
Mats A. Granskog ◽  
Mathias Middelboe
Keyword(s):  
Organic Matter ◽  
Dissolved Organic Matter ◽  
Microbial Production ◽  
Fluorescent Dissolved Organic Matter
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