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dc.contributor.authorMancin, Nicoletta
dc.contributor.authorDarling, Kate
dc.date.accessioned2016-09-05T23:32:30Z
dc.date.available2016-09-05T23:32:30Z
dc.date.issued2015-10-15
dc.identifier.citationMancin , N & Darling , K 2015 , ' Morphological abnormalities of planktonic foraminiferal tests in the SW pacific ocean over the last 550ky ' , Marine Micropaleontology , vol. 120 , pp. 1-19 . https://doi.org/10.1016/j.marmicro.2015.08.003en
dc.identifier.issn0377-8398
dc.identifier.otherPURE: 215400794
dc.identifier.otherPURE UUID: 6228ae00-05e0-4f2d-93ec-81b0adce5c79
dc.identifier.otherRIS: urn:32216041D1FE03417F6429B7BCE46750
dc.identifier.otherScopus: 84941265930
dc.identifier.otherWOS: 000365064900001
dc.identifier.urihttps://hdl.handle.net/10023/9431
dc.descriptionThis project was funded by “FAR 2012-2014” grants of the University of Pavia (Italy).en
dc.description.abstractThe paper focuses on the occurrence of morphologically abnormal specimens of planktonic foraminifera observed over the last 550ky in IMAGES core MD 97-2114 (East of New Zealand, SW Pacific). Abnormal tests occurred throughout the entire record in all the morphospecies characterising the assemblages but were relatively rare, with percentages not exceeding 1.5% of the total assemblage. No mass abnormality events were found. A range of malformations were observed from slight deformity with smaller or overdeveloped chambers to more severe deformity, with misplaced chambers, distorted spirals or double tests forming twinned individuals. They exhibited several different categories of morphological abnormalities, even within the same sample. Test abnormalities were most abundant in the morphospecies Globorotalia inflata, Globigerina bulloides and Orbulina universa and were characterised by a long-term decreasing trend up core with an alternating % abundance pattern at the glacial to interglacial scale between MIS 14 to MIS 8, recording the highest percentages during the interglacials. Normalised total abundance and abnormal abundance curves co-varied very closely for G. bulloides and O. universa, but for G. inflata two opposing excursions were observed during MIS 13 and 6 which may be linked to water column states. Although abnormal numbers were proportionately low, there appears to be a “natural” background number of malformations in the G. inflata population through time. There was no relationship between volcanic ash production and test abnormalities.
dc.language.isoeng
dc.relation.ispartofMarine Micropaleontologyen
dc.rightsCopyright © 2015 Published by Elsevier B.V. This work is made available online in accordance with the publisher’s policies. This is the author created, accepted version manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at https://dx.doi.org/10.1016/j.marmicro.2015.08.003en
dc.subjectPlanktonic foraminiferaen
dc.subjectAbnormal testen
dc.subjectEnvironmental stressorsen
dc.subjectPleistocene, SW pacificen
dc.subjectGE Environmental Sciencesen
dc.subjectDASen
dc.subject.lccGEen
dc.titleMorphological abnormalities of planktonic foraminiferal tests in the SW pacific ocean over the last 550kyen
dc.typeJournal articleen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews. School of Geography and Geosciencesen
dc.identifier.doihttps://doi.org/10.1016/j.marmicro.2015.08.003
dc.description.statusPeer revieweden
dc.date.embargoedUntil2016-09-05


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