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dc.contributor.authorJonkers, L
dc.contributor.authorMix, A
dc.contributor.authorVoelker, A
dc.contributor.authorRisebrobakken, B
dc.contributor.authorSmart, CW
dc.contributor.authorIvanova, E
dc.contributor.authorArellano-Torres, E
dc.contributor.authorEynaud, F
dc.contributor.authorNaoufel, H
dc.contributor.authorMax, L
dc.contributor.authorRossignol, L
dc.contributor.authorSimon, MH
dc.contributor.authorMartins, MVA
dc.contributor.authorPetró, S
dc.contributor.authorCaley, T
dc.contributor.authorDokken, T
dc.contributor.authorHoward, W
dc.contributor.authorKucera, M
dc.date.accessioned2024-05-13T15:04:23Z
dc.date.available2024-05-13T15:04:23Z
dc.date.issued2024-04-10
dc.identifier.issn2052-4463
dc.identifier.issn2052-4463
dc.identifier.other361
dc.identifier.urihttps://pearl.plymouth.ac.uk/handle/10026.1/22495
dc.description.abstract

Species assemblage composition of marine microfossils offers the possibility to investigate ecological and climatological change on time scales inaccessible using conventional observations. Planktonic foraminifera - calcareous zooplankton - have an excellent fossil record and are used extensively in palaeoecology and palaeoceanography. During the Last Glacial Maximum (LGM; 19,000 – 23,000 years ago), the climate was in a radically different state. This period is therefore a key target to investigate climate and biodiversity under different conditions than today. Studying LGM climate and ecosystems indeed has a long history, yet the most recent global synthesis of planktonic foraminifera assemblage composition is now nearly two decades old. Here we present the ForCenS-LGM dataset with 2,365 species assemblage samples collected using standardised methods and with harmonised taxonomy. The data originate from marine sediments from 664 sites and present a more than 50% increase in coverage compared to previous work. The taxonomy is compatible with the most recent global core top dataset, enabling direct investigation of temporal changes in foraminifera biogeography and facilitating seawater temperature reconstructions.

dc.format.extent361-
dc.format.mediumElectronic
dc.languageen
dc.publisherSpringer Science and Business Media LLC
dc.subjectAnimals
dc.subjectBiodiversity
dc.subjectEcosystem
dc.subjectForaminifera
dc.subjectZooplankton
dc.subjectFossils
dc.titleForCenS-LGM: a dataset of planktonic foraminifera species assemblage composition for the Last Glacial Maximum
dc.typejournal-article
dc.typeArticle
plymouth.author-urlhttps://www.ncbi.nlm.nih.gov/pubmed/38600091
plymouth.issue1
plymouth.volume11
plymouth.publisher-urlhttp://dx.doi.org/10.1038/s41597-024-03166-7
plymouth.publication-statusPublished online
plymouth.journalScientific Data
dc.identifier.doi10.1038/s41597-024-03166-7
plymouth.organisational-group|Plymouth
plymouth.organisational-group|Plymouth|Research Groups
plymouth.organisational-group|Plymouth|Faculty of Science and Engineering
plymouth.organisational-group|Plymouth|Faculty of Science and Engineering|School of Geography, Earth and Environmental Sciences
plymouth.organisational-group|Plymouth|Research Groups|Marine Institute
plymouth.organisational-group|Plymouth|REF 2021 Researchers by UoA
plymouth.organisational-group|Plymouth|Users by role
plymouth.organisational-group|Plymouth|Users by role|Current Academic staff
plymouth.organisational-group|Plymouth|REF 2021 Researchers by UoA|UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group|Plymouth|REF 2029 Researchers by UoA
plymouth.organisational-group|Plymouth|REF 2029 Researchers by UoA|UoA07 Earth Systems and Environmental Sciences
dc.publisher.placeEngland
dcterms.dateAccepted2024-03-20
dc.date.updated2024-05-13T15:04:22Z
dc.rights.embargodate2024-5-18
dc.identifier.eissn2052-4463
rioxxterms.versionofrecord10.1038/s41597-024-03166-7


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