Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution
S1: Study species Globoconella puncticulata (a) and Truncorotalia crassaformis (b). The scale bars represent 100 μm. S2: Map of study site IODP Site U1313 in the North Atlantic. S3: Autocorrelation plots for traits of Globoconella puncticulata showing autocorrelation in the original time series (a-c...
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ftdatacite:10.6084/m9.figshare.6743357.v1 2023-05-15T17:33:32+02:00 Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution Anieke Brombacher Wilson, Paul A. Bailey, Ian Ezard, Thomas H. G. 2018 https://dx.doi.org/10.6084/m9.figshare.6743357.v1 https://rs.figshare.com/articles/Supplementary_figures_S1-S5_from_Temperature_is_a_poor_proxy_for_synergistic_climate_forcing_of_plankton_evolution/6743357/1 unknown The Royal Society https://dx.doi.org/10.1098/rspb.2018.0665 https://dx.doi.org/10.6084/m9.figshare.6743357 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Evolutionary Biology FOS Biological sciences Environmental Science 40308 Palaeontology incl. Palynology FOS Earth and related environmental sciences Text article-journal Journal contribution ScholarlyArticle 2018 ftdatacite https://doi.org/10.6084/m9.figshare.6743357.v1 https://doi.org/10.1098/rspb.2018.0665 https://doi.org/10.6084/m9.figshare.6743357 2021-11-05T12:55:41Z S1: Study species Globoconella puncticulata (a) and Truncorotalia crassaformis (b). The scale bars represent 100 μm. S2: Map of study site IODP Site U1313 in the North Atlantic. S3: Autocorrelation plots for traits of Globoconella puncticulata showing autocorrelation in the original time series (a-c) but not in the first differences (d-f). S4: Autocorrelation plots for traits of Truncorotalia crassaformis showing autocorrelation in the original time series (a-c) but not in the first differences (d-f ). Only area in T. crassaformis still contained a small amount of autocorrelation in the first differences time series. However, comparison of two Generalized Least Squares models with and without autocorrelation (by setting the continuous auto-correlation parameter phi=0.3 and phi=0.1, which converges to 0 under maximum likelihood, respectively) show lower AIC values for the model without autocorrelation, implying that the model with temporal autocorrelation is actually a poorer fit to the data than that without. S5: ΔAIC values showing the added relative importance of each environmental parameter or combination of parameters to the total model. Text North Atlantic DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
language |
unknown |
topic |
Evolutionary Biology FOS Biological sciences Environmental Science 40308 Palaeontology incl. Palynology FOS Earth and related environmental sciences |
spellingShingle |
Evolutionary Biology FOS Biological sciences Environmental Science 40308 Palaeontology incl. Palynology FOS Earth and related environmental sciences Anieke Brombacher Wilson, Paul A. Bailey, Ian Ezard, Thomas H. G. Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution |
topic_facet |
Evolutionary Biology FOS Biological sciences Environmental Science 40308 Palaeontology incl. Palynology FOS Earth and related environmental sciences |
description |
S1: Study species Globoconella puncticulata (a) and Truncorotalia crassaformis (b). The scale bars represent 100 μm. S2: Map of study site IODP Site U1313 in the North Atlantic. S3: Autocorrelation plots for traits of Globoconella puncticulata showing autocorrelation in the original time series (a-c) but not in the first differences (d-f). S4: Autocorrelation plots for traits of Truncorotalia crassaformis showing autocorrelation in the original time series (a-c) but not in the first differences (d-f ). Only area in T. crassaformis still contained a small amount of autocorrelation in the first differences time series. However, comparison of two Generalized Least Squares models with and without autocorrelation (by setting the continuous auto-correlation parameter phi=0.3 and phi=0.1, which converges to 0 under maximum likelihood, respectively) show lower AIC values for the model without autocorrelation, implying that the model with temporal autocorrelation is actually a poorer fit to the data than that without. S5: ΔAIC values showing the added relative importance of each environmental parameter or combination of parameters to the total model. |
format |
Text |
author |
Anieke Brombacher Wilson, Paul A. Bailey, Ian Ezard, Thomas H. G. |
author_facet |
Anieke Brombacher Wilson, Paul A. Bailey, Ian Ezard, Thomas H. G. |
author_sort |
Anieke Brombacher |
title |
Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution |
title_short |
Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution |
title_full |
Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution |
title_fullStr |
Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution |
title_full_unstemmed |
Supplementary figures S1-S5 from Temperature is a poor proxy for synergistic climate forcing of plankton evolution |
title_sort |
supplementary figures s1-s5 from temperature is a poor proxy for synergistic climate forcing of plankton evolution |
publisher |
The Royal Society |
publishDate |
2018 |
url |
https://dx.doi.org/10.6084/m9.figshare.6743357.v1 https://rs.figshare.com/articles/Supplementary_figures_S1-S5_from_Temperature_is_a_poor_proxy_for_synergistic_climate_forcing_of_plankton_evolution/6743357/1 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1098/rspb.2018.0665 https://dx.doi.org/10.6084/m9.figshare.6743357 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.6743357.v1 https://doi.org/10.1098/rspb.2018.0665 https://doi.org/10.6084/m9.figshare.6743357 |
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