Fig 1 -

Effects of Fe reduction ( +Fe vs Control ) and pCO 2 increase ( 190 vs 290 ) on (A) growth rate ( μ ), (B) POC production, (C) PON production and (D) BSi production in the four treatments of P . subcurvata ( +Fe 190 , Control 190 , +Fe 290 and Control 290 ) at the end of the experiment. The values r...

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Bibliographic Details
Main Authors: Anna Pagnone (11824679), Florian Koch (6508592), Franziska Pausch (7387982), Scarlett Trimborn (487685)
Format: Still Image
Language:unknown
Published: 2021
Subjects:
Molecular Biology
Evolutionary Biology
Ecology
Developmental Biology
Marine Biology
Cancer
Infectious Diseases
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
thicker silica shells
particulate organic carbon
negative effect caused
increased dust deposition
form prominent blooms
290 &# 956
div >< p
>
thus contributing
lower atmospheric pco
290 μatm pco
interglacial climatic conditions
190 &# 956
nitzschia subcurvata </
interglacial ocean conditions
southern ocean diatom
low fe availability
favored poc production
higher fe availability
southern ocean
interglacial conditions
subcurvata </
p </
low pco
higher pco
interglacial times
known
higher degree
different pco
glacial ocean
glacial conditions
fe input
fe deficiency
fe addition
similar rates
results show
primary production
poc production
influences growth
flourished better
diatom grew
diatom could
combined effects
Southern Ocean
Online Access:https://doi.org/10.1371/journal.pone.0260649.g001
Description
Summary:Effects of Fe reduction ( +Fe vs Control ) and pCO 2 increase ( 190 vs 290 ) on (A) growth rate ( μ ), (B) POC production, (C) PON production and (D) BSi production in the four treatments of P . subcurvata ( +Fe 190 , Control 190 , +Fe 290 and Control 290 ) at the end of the experiment. The values represent the means ± SD (n = 3). Different letters indicate significant differences between treatments (p < 0.05).

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