BACTERIAL SURFACE INTERACTIONS WITH NASCENT SUBCELLULAR PARTICLES: IMPORTANCE FOR THE UPPER OCEAN CARBON CYCLE The grant to the Scripps Institution of Oceanography supports investigating how heterotrophic bacteria respond to nascent cellular debris and virus particles. By combining new microscopy tools with molecular and isotope techniques, this project aims to advance understanding of the mechanisms that drive biogeochemical cycling of phytoplankton lysate in the surface ocean. AFM micrographs of model lysate paticles (E. coli ribosomes) adsorbed onto mica (A) and with marine bacterium SWAT3 (Vibrio sp.) (C and D respectively).
Project Data Further information and data can be obtained by contacting Dr. Farooq Azam: fazam@ucsd.edu Cellular particles in natural assemblages
Related to the investigation of the viral degradation by bacteria, the viral attachments to non-host bacteria was investigated by microscopy. We incubated two isolated viruses with four bacteria in artificial seawater and the attachments between them was quantified. The attachment was occurred in every combination of virus and bacteria and the rates were relatively different depending on the combinations.
Marine bacteria have been shown to rapidly colonize and degrade phytoplankton detritus which plays a significant role in ocean carbon export. Here, we studied the the mechanisms of bacterial colonization and degradation of particulate organic matter, by means of observation of bacterial interactions with dead dinoflagellate (Pyrocystis fusiform) cells at the microscale.
(Please contact Dr. Azam for addition information about AFM data) Representative height image of seawater with particle aggregates designated. AFM micrograph (height image) of marine microbes (blue circles) associated with colloidal particles and larger structures. Microbes are frequently observed with attached particles (white arrows) on their surface. An example of microbes associated with larger structures (discarded larvacean house), which is partially covered with colloidal particles. Bacterioplankton drawdown of coral mass-spawned organic matter
Each year in the Caribbean, coral of the genus Orbicella engage in highly predictable mass-spawning reproductive events. Here, we joined a team from PennState University (http://medinalab.org/new/) to investigate microbial response to a pulse of spawn derived organic matter using a combination of field and microcosm studies. We show that the total organic carbon (TOC) concentration was elevated to 515 µMC and that 68% of it degraded within just 66 hr. In collaboration with The University of Tokyo (http://www.aori.u-tokyo.ac.jp/english/index.html), we also sequence bromodeoxyuridine labeled 16S-rRNA genes to determine the active microbial taxa responding to the event and provide evidence that these active taxa were primarily responsible for the measured TOC degradation. Furthermore, we used Fourier transform ion cyclotron mass spectrometry (FT-ICR-MS) in collaboration with the Alfred Wegener Institute (https://www.awi.de/en/about-us/organisation/staff/boris-koch.html) to characterize the dissolved organic matter pool and show the presence of three unique molecular formulas to this mass-spawning event. Time-lapse imaging of microbial surfaces changes and structure dissolution AFM time-lapse visualization of the dynamic surfaces of live Pseudoalteromonas sp. TW7 cells. Time-lapse visualization of the microbial surface changes of an individual Alteromonas sp. ALTSIO cell. Height image on the left with processed image visualizing convex bumps on the right. AFM time-lapse visualization of ALTSIO cells exposed to E. coli ribosomes in solution. AFM visualization of dissolution of flagella (SWAT-3) on bare mica. Previous Grant CLOSELY INTERACTING MICROBES AS HOTSPOTS OF BIOGEOCHEMICAL ACTIVITY The grant to the Scripps Institution of Oceanography supports investigating how closely coupled marine microorganisms interact physically and exchange nutrient molecules. By combining new microscopy tools with molecular and isotope techniques, this project aims to advance understanding of the mechanisms that drive biogeochemical cycles in the surface ocean.
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