Image4.TIF

We have assessed how varying CO 2 (180, 380, and 720 μatm) and growth light intensity (40 and 400 μmol photons m −2 s −1 ) affected Trichodesmium erythraeum IMS101 growth and photophysiology over free iron (Fe′) concentrations between 20 and 9,600 pM. We found significant iron dependencies of growth...

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Bibliographic Details
Main Authors: Tobias G. Boatman, Kevin Oxborough, Martha Gledhill, Tracy Lawson, Richard J. Geider
Format: Still Image
Language:unknown
Published: 2018
Subjects:
CO2
Online Access:https://doi.org/10.3389/fmicb.2018.00624.s004
https://figshare.com/articles/Image4_TIF/6119636
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spelling ftfrontimediafig:oai:figshare.com:article/6119636 2023-05-15T17:51:24+02:00 Image4.TIF Tobias G. Boatman Kevin Oxborough Martha Gledhill Tracy Lawson Richard J. Geider 2018-04-10T04:18:41Z https://doi.org/10.3389/fmicb.2018.00624.s004 https://figshare.com/articles/Image4_TIF/6119636 unknown doi:10.3389/fmicb.2018.00624.s004 https://figshare.com/articles/Image4_TIF/6119636 CC BY 4.0 CC-BY Microbiology Microbial Genetics Microbial Ecology Mycology Trichodesmium erythraeum Cyanobacteria ocean acidification CO2 iron limitation light intensity fluorescence light curves electron transport rates Image Figure 2018 ftfrontimediafig https://doi.org/10.3389/fmicb.2018.00624.s004 2018-04-11T22:57:07Z We have assessed how varying CO 2 (180, 380, and 720 μatm) and growth light intensity (40 and 400 μmol photons m −2 s −1 ) affected Trichodesmium erythraeum IMS101 growth and photophysiology over free iron (Fe′) concentrations between 20 and 9,600 pM. We found significant iron dependencies of growth rate and the initial slope and maximal relative PSII electron transport rates (rP m ). Under iron-limiting concentrations, high-light increased growth rates and rP m possibly indicating a lower allocation of resources to iron-containing photosynthetic proteins. Higher CO 2 increased growth rates across all iron concentrations, enabled growth to occur at lower Fe′ concentrations, increased rP m and lowered the iron half saturation constants for growth (K m ). We attribute these CO 2 responses to the operation of the CCM and the ATP spent/saved for CO 2 uptake and transport at low and high CO 2 , respectively. It seems reasonable to conclude that T. erythraeum IMS101 can exhibit a high degree of phenotypic plasticity in response to CO 2 , light intensity and iron-limitation. These results are important given predictions of increased dissolved CO 2 and water column stratification (i.e., higher light exposures) over the coming decades. Still Image Ocean acidification Frontiers: Figshare
institution Open Polar
collection Frontiers: Figshare
op_collection_id ftfrontimediafig
language unknown
topic Microbiology
Microbial Genetics
Microbial Ecology
Mycology
Trichodesmium erythraeum
Cyanobacteria
ocean acidification
CO2
iron limitation
light intensity
fluorescence light curves
electron transport rates
spellingShingle Microbiology
Microbial Genetics
Microbial Ecology
Mycology
Trichodesmium erythraeum
Cyanobacteria
ocean acidification
CO2
iron limitation
light intensity
fluorescence light curves
electron transport rates
Tobias G. Boatman
Kevin Oxborough
Martha Gledhill
Tracy Lawson
Richard J. Geider
Image4.TIF
topic_facet Microbiology
Microbial Genetics
Microbial Ecology
Mycology
Trichodesmium erythraeum
Cyanobacteria
ocean acidification
CO2
iron limitation
light intensity
fluorescence light curves
electron transport rates
description We have assessed how varying CO 2 (180, 380, and 720 μatm) and growth light intensity (40 and 400 μmol photons m −2 s −1 ) affected Trichodesmium erythraeum IMS101 growth and photophysiology over free iron (Fe′) concentrations between 20 and 9,600 pM. We found significant iron dependencies of growth rate and the initial slope and maximal relative PSII electron transport rates (rP m ). Under iron-limiting concentrations, high-light increased growth rates and rP m possibly indicating a lower allocation of resources to iron-containing photosynthetic proteins. Higher CO 2 increased growth rates across all iron concentrations, enabled growth to occur at lower Fe′ concentrations, increased rP m and lowered the iron half saturation constants for growth (K m ). We attribute these CO 2 responses to the operation of the CCM and the ATP spent/saved for CO 2 uptake and transport at low and high CO 2 , respectively. It seems reasonable to conclude that T. erythraeum IMS101 can exhibit a high degree of phenotypic plasticity in response to CO 2 , light intensity and iron-limitation. These results are important given predictions of increased dissolved CO 2 and water column stratification (i.e., higher light exposures) over the coming decades.
format Still Image
author Tobias G. Boatman
Kevin Oxborough
Martha Gledhill
Tracy Lawson
Richard J. Geider
author_facet Tobias G. Boatman
Kevin Oxborough
Martha Gledhill
Tracy Lawson
Richard J. Geider
author_sort Tobias G. Boatman
title Image4.TIF
title_short Image4.TIF
title_full Image4.TIF
title_fullStr Image4.TIF
title_full_unstemmed Image4.TIF
title_sort image4.tif
publishDate 2018
url https://doi.org/10.3389/fmicb.2018.00624.s004
https://figshare.com/articles/Image4_TIF/6119636
genre Ocean acidification
genre_facet Ocean acidification
op_relation doi:10.3389/fmicb.2018.00624.s004
https://figshare.com/articles/Image4_TIF/6119636
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.3389/fmicb.2018.00624.s004
_version_ 1766158539923914752