Diatom specific growth rates based on cell concentrations and PDMPO staining

While in culture, specific growth rate (μ) can be easily determined through cell counts (N0 and Nt). This is not the case for incubations with natural assemblages, where grazers and other processes lead to cell loss and consequently an underestimation of Nt. Incubations with [2-(4-pyridyl)-5{[4-dime...

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Main Authors: Husmann, Eva, Klaas, Christine
Format: Dataset
Language:English
Published: PANGAEA 2023
Subjects:
HN
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.954982
https://doi.org/10.1594/PANGAEA.954982
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.954982
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.954982 2024-09-15T18:17:03+00:00 Diatom specific growth rates based on cell concentrations and PDMPO staining Husmann, Eva Klaas, Christine MEDIAN LATITUDE: -27.053402 * MEDIAN LONGITUDE: 21.788440 * SOUTH-BOUND LATITUDE: -69.000000 * WEST-BOUND LONGITUDE: 0.099790 * NORTH-BOUND LATITUDE: 78.953000 * EAST-BOUND LONGITUDE: 75.000000 * DATE/TIME START: 2018-05-10T00:00:00 * DATE/TIME END: 2018-12-31T12:12:00 * MINIMUM ELEVATION: -4679.0 m * MAXIMUM ELEVATION: -4500.0 m 2023 text/tab-separated-values, 194 data points https://doi.pangaea.de/10.1594/PANGAEA.954982 https://doi.org/10.1594/PANGAEA.954982 en eng PANGAEA https://doi.org/10.1594/PANGAEA.954985 Husmann, Eva; Klaas, Christine (2022): Testing the use of the silica deposition fluorescent probe PDMPO to estimate in situ growth rates of diatoms. Limnology and Oceanography-Methods, 20(9), 568-580, https://doi.org/10.1002/lom3.10505 Utermöhl, H (1958): Zur Vervollkommnung der quantitativen Phytoplankton-Methodik. Mitteilungen der Internationalen Vereinigung für Theoretische und Angewandte Limnologie, 9, 1-38 https://doi.pangaea.de/10.1594/PANGAEA.954982 https://doi.org/10.1594/PANGAEA.954982 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess biological oceanography Calculated Date/time start experiment diatoms Epifluorescence microscopy Event label Experimental treatment Hand net HN Incubation duration in situ growth rates Kongsfjorden_CC_Sed Kongsfjorden Spitsbergen Arctic Laboratory experiment Light microscopy (Utermöhl 1958) method Phytoplankton Phytoplankton growth rate specific Polarstern Prydz_Bay_CS-624 Prydz Bay PS117 PS117_22-6 South Atlantic Ocean Species Specific growth rate standard deviation Strain Taxon/taxa unique identification unique identification (Semantic URI) unique identification (URI) Temperature water Treatment: light intensity Type of study dataset 2023 ftpangaea https://doi.org/10.1594/PANGAEA.95498210.1594/PANGAEA.95498510.1002/lom3.10505 2024-07-24T02:31:43Z While in culture, specific growth rate (μ) can be easily determined through cell counts (N0 and Nt). This is not the case for incubations with natural assemblages, where grazers and other processes lead to cell loss and consequently an underestimation of Nt. Incubations with [2-(4-pyridyl)-5{[4-dimethylaminoethyl-aminocarbamoyl)-methoxy]phenyl}oxazole] (PDMPO) overcomes this issue by allowing the determination of N0 (Nt=N0×e^(μt) (Eq. 1)) based on the relative proportion of PDMPO stained cells (newly divided) and unstained cell at the end of an incubation as follows: Given Nt, the total cell number of a species from a subsample at a time t after PDMPO addition. Nt=nt+nt', with nt the total number of non-(PDMPO) stained cells of the species in the same subsample (cells that did not divide yet), and nt' the total number of cells with one PDMPO stained valve (cells issued from the first division after PDMPO addition to the culture media). All things being equal, the population (N0) at the time when PDMPO was added that gave rise to Nt should be N0=nt+((nt')/2)=Nt-((nt')/2) (Eq. 2). Growth rates from cells counts were estimated using (Eq. 1), while growth rates using PDMPO were calculated from the number of non-stained (nt), half-stained (nt') and fully stained (nt'') cells using μ[d-1]=ln((nt+nt')/(nt+(nt')/2))×(1/t) (Eq. 3) or μ[d-1]=ln((nt'+nt'')/((nt')/2))×(1/t) (Eq. 4). Cells attached to each other (potentially in the final phase of division) were also considered as non-stained, half-stained and fully-stained individuals, respectively, based on the presence/absence of a PDMPO signal on the valves. Dataset Kongsfjord* Kongsfjorden Phytoplankton Prydz Bay South Atlantic Ocean Spitsbergen PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(0.099790,75.000000,78.953000,-69.000000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic biological oceanography
Calculated
Date/time start
experiment
diatoms
Epifluorescence microscopy
Event label
Experimental treatment
Hand net
HN
Incubation duration
in situ growth rates
Kongsfjorden_CC_Sed
Kongsfjorden
Spitsbergen
Arctic
Laboratory experiment
Light microscopy (Utermöhl 1958)
method
Phytoplankton
Phytoplankton growth rate
specific
Polarstern
Prydz_Bay_CS-624
Prydz Bay
PS117
PS117_22-6
South Atlantic Ocean
Species
Specific growth rate
standard deviation
Strain
Taxon/taxa
unique identification
unique identification (Semantic URI)
unique identification (URI)
Temperature
water
Treatment: light intensity
Type of study
spellingShingle biological oceanography
Calculated
Date/time start
experiment
diatoms
Epifluorescence microscopy
Event label
Experimental treatment
Hand net
HN
Incubation duration
in situ growth rates
Kongsfjorden_CC_Sed
Kongsfjorden
Spitsbergen
Arctic
Laboratory experiment
Light microscopy (Utermöhl 1958)
method
Phytoplankton
Phytoplankton growth rate
specific
Polarstern
Prydz_Bay_CS-624
Prydz Bay
PS117
PS117_22-6
South Atlantic Ocean
Species
Specific growth rate
standard deviation
Strain
Taxon/taxa
unique identification
unique identification (Semantic URI)
unique identification (URI)
Temperature
water
Treatment: light intensity
Type of study
Husmann, Eva
Klaas, Christine
Diatom specific growth rates based on cell concentrations and PDMPO staining
topic_facet biological oceanography
Calculated
Date/time start
experiment
diatoms
Epifluorescence microscopy
Event label
Experimental treatment
Hand net
HN
Incubation duration
in situ growth rates
Kongsfjorden_CC_Sed
Kongsfjorden
Spitsbergen
Arctic
Laboratory experiment
Light microscopy (Utermöhl 1958)
method
Phytoplankton
Phytoplankton growth rate
specific
Polarstern
Prydz_Bay_CS-624
Prydz Bay
PS117
PS117_22-6
South Atlantic Ocean
Species
Specific growth rate
standard deviation
Strain
Taxon/taxa
unique identification
unique identification (Semantic URI)
unique identification (URI)
Temperature
water
Treatment: light intensity
Type of study
description While in culture, specific growth rate (μ) can be easily determined through cell counts (N0 and Nt). This is not the case for incubations with natural assemblages, where grazers and other processes lead to cell loss and consequently an underestimation of Nt. Incubations with [2-(4-pyridyl)-5{[4-dimethylaminoethyl-aminocarbamoyl)-methoxy]phenyl}oxazole] (PDMPO) overcomes this issue by allowing the determination of N0 (Nt=N0×e^(μt) (Eq. 1)) based on the relative proportion of PDMPO stained cells (newly divided) and unstained cell at the end of an incubation as follows: Given Nt, the total cell number of a species from a subsample at a time t after PDMPO addition. Nt=nt+nt', with nt the total number of non-(PDMPO) stained cells of the species in the same subsample (cells that did not divide yet), and nt' the total number of cells with one PDMPO stained valve (cells issued from the first division after PDMPO addition to the culture media). All things being equal, the population (N0) at the time when PDMPO was added that gave rise to Nt should be N0=nt+((nt')/2)=Nt-((nt')/2) (Eq. 2). Growth rates from cells counts were estimated using (Eq. 1), while growth rates using PDMPO were calculated from the number of non-stained (nt), half-stained (nt') and fully stained (nt'') cells using μ[d-1]=ln((nt+nt')/(nt+(nt')/2))×(1/t) (Eq. 3) or μ[d-1]=ln((nt'+nt'')/((nt')/2))×(1/t) (Eq. 4). Cells attached to each other (potentially in the final phase of division) were also considered as non-stained, half-stained and fully-stained individuals, respectively, based on the presence/absence of a PDMPO signal on the valves.
format Dataset
author Husmann, Eva
Klaas, Christine
author_facet Husmann, Eva
Klaas, Christine
author_sort Husmann, Eva
title Diatom specific growth rates based on cell concentrations and PDMPO staining
title_short Diatom specific growth rates based on cell concentrations and PDMPO staining
title_full Diatom specific growth rates based on cell concentrations and PDMPO staining
title_fullStr Diatom specific growth rates based on cell concentrations and PDMPO staining
title_full_unstemmed Diatom specific growth rates based on cell concentrations and PDMPO staining
title_sort diatom specific growth rates based on cell concentrations and pdmpo staining
publisher PANGAEA
publishDate 2023
url https://doi.pangaea.de/10.1594/PANGAEA.954982
https://doi.org/10.1594/PANGAEA.954982
op_coverage MEDIAN LATITUDE: -27.053402 * MEDIAN LONGITUDE: 21.788440 * SOUTH-BOUND LATITUDE: -69.000000 * WEST-BOUND LONGITUDE: 0.099790 * NORTH-BOUND LATITUDE: 78.953000 * EAST-BOUND LONGITUDE: 75.000000 * DATE/TIME START: 2018-05-10T00:00:00 * DATE/TIME END: 2018-12-31T12:12:00 * MINIMUM ELEVATION: -4679.0 m * MAXIMUM ELEVATION: -4500.0 m
long_lat ENVELOPE(0.099790,75.000000,78.953000,-69.000000)
genre Kongsfjord*
Kongsfjorden
Phytoplankton
Prydz Bay
South Atlantic Ocean
Spitsbergen
genre_facet Kongsfjord*
Kongsfjorden
Phytoplankton
Prydz Bay
South Atlantic Ocean
Spitsbergen
op_relation https://doi.org/10.1594/PANGAEA.954985
Husmann, Eva; Klaas, Christine (2022): Testing the use of the silica deposition fluorescent probe PDMPO to estimate in situ growth rates of diatoms. Limnology and Oceanography-Methods, 20(9), 568-580, https://doi.org/10.1002/lom3.10505
Utermöhl, H (1958): Zur Vervollkommnung der quantitativen Phytoplankton-Methodik. Mitteilungen der Internationalen Vereinigung für Theoretische und Angewandte Limnologie, 9, 1-38
https://doi.pangaea.de/10.1594/PANGAEA.954982
https://doi.org/10.1594/PANGAEA.954982
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.95498210.1594/PANGAEA.95498510.1002/lom3.10505
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