dc.contributor.author | Yasuhara, Moriaki | |
dc.contributor.author | Wei, Chih-Lin | |
dc.contributor.author | Kucera, Michal | |
dc.contributor.author | Costello, Mark John | |
dc.contributor.author | Tittensor, Derek P. | |
dc.contributor.author | Kiessling, Wolfgang | |
dc.contributor.author | Bonebrake, Timothy C. | |
dc.contributor.author | Tabor, Clay | |
dc.contributor.author | Feng, Ran | |
dc.contributor.author | Baselga, Andrés | |
dc.contributor.author | Kretschmer, Kerstin | |
dc.contributor.author | Kusumoto, Buntarou | |
dc.contributor.author | Kubota, Yasuhiro | |
dc.date.accessioned | 2021-01-19T12:24:44Z | |
dc.date.available | 2021-01-19T12:24:44Z | |
dc.date.created | 2020-11-18T00:23:28Z | |
dc.date.issued | 2020 | |
dc.identifier.citation | Yasuhara, M., Wei, C.-L., Kucera, M., Costello, M. J., Tittensor, D. P., Kiessling, W., Bonebrake, T. C., Tabor, C. R., Feng, R., Baselga, A., Kretschmer, K., Kusumoto, B. & Kubota, Y. (2020). Past and future decline of tropical pelagic biodiversity. Proceedings of the National Academy of Sciences of the United States of America, 117(23), 12891-12896. doi: | en_US |
dc.identifier.issn | 1091-6490 | |
dc.identifier.uri | https://hdl.handle.net/11250/2723688 | |
dc.description | Author's accepted version (postprint). | en_US |
dc.description | This is an Accepted Manuscript of an article published by the National Academy of Sciences in PNAS on 26/05/2020. | |
dc.description | Available online: https://www.pnas.org/content/pnas/117/23/12891.full.pdf | |
dc.description.abstract | A major research question concerning global pelagic biodiversity remains unanswered: when did the apparent tropical biodiversity depression (i.e., bimodality of latitudinal diversity gradient [LDG]) begin? The bimodal LDG may be a consequence of recent ocean warming or of deep-time evolutionary speciation and extinction processes. Using rich fossil datasets of planktonic foraminifers, we show here that a unimodal (or only weakly bimodal) diversity gradient, with a plateau in the tropics, occurred during the last ice age and has since then developed into a bimodal gradient through species distribution shifts driven by postglacial ocean warming. The bimodal LDG likely emerged before the Anthropocene and industrialization, and perhaps ∼15,000 y ago, indicating a strong environmental control of tropical diversity even before the start of anthropogenic warming. However, our model projections suggest that future anthropogenic warming further diminishes tropical pelagic diversity to a level not seen in millions of years. | en_US |
dc.language.iso | eng | en_US |
dc.publisher | National Academy of Sciences | en_US |
dc.title | Past and future decline of tropical pelagic biodiversity | en_US |
dc.type | Peer reviewed | en_US |
dc.type | Journal article | en_US |
dc.description.version | acceptedVersion | en_US |
dc.subject.nsi | VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Marinbiologi: 497 | en_US |
dc.subject.nsi | VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Økologi: 488 | en_US |
dc.subject.nsi | VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Stratigrafi og paleontologi: 461 | en_US |
dc.subject.nsi | VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Zoogeografi: 486 | en_US |
dc.source.pagenumber | 12891-12896 | en_US |
dc.source.volume | 117 | en_US |
dc.source.journal | Proceedings of the National Academy of Sciences of the United States of America | en_US |
dc.source.issue | 23 | en_US |
dc.identifier.doi | 10.1073/pnas.1916923117 | |
dc.identifier.cristin | 1848986 | |