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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00004070naa a2200577 4500
001oai:DiVA.org:su-163566
003SwePub
008190115s2018 | |||||||||||000 ||eng|
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1635662 URI
0247 a https://doi.org/10.1016/j.revmic.2018.10.0012 DOI
040 a (SwePub)su
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a for2 swepub-publicationtype
1001 a Schiebel, Ralf4 aut
2451 0a Advances in planktonic foraminifer research :b New perspectives for paleoceanography
264 1b Elsevier BV,c 2018
338 a print2 rdacarrier
520 a Planktonic foraminifer tests are major archives of environmental change and provide a multitude of proxies in paleoceanography and paleoclimatology. The application of such proxies is contingent upon a collaborative effort to better understand how the living organisms record the properties of their environment and how the resulting signals are recorded in marine sediments. In this contribution, we provide a review of the rapidly developing sub-fields of research, where new advances have been made possibleby technological developments, and by cross-disciplinary work of the scientific community. Following brief historical overviews of the sub-fields, we discuss the latest advances in planktonic foraminifer research and highlight the resulting new perspectives in ocean and climate research. Natural classification based on consistent species concepts forms the basis for analysis of any foraminifer-derived proxy. New approaches in taxonomy and phylogeny of Cenozoic planktonic foraminifers (Section 2) are presented, highlighting new perspectives on sensitivity and response of planktonic foraminifers to the changing climate and environment (Section 4). Calibration of foraminifer-specific data and environmental parameters is improving along with the technical development of probes and the access to samples from the natural environment (Section 3), enhancing our understanding of the ever-changing climate and ocean system. Comprehension of sedimentation and flux dynamics facilitates maximum gain of information from fossil assemblages (Section 5). Subtle changes in the physical (e.g., temperature), chemical (e.g., pH), and biological (e.g., food) conditions of ambient seawater affect the abundance of species and composition of assemblages as well as the chemical composition of the foraminifer shell and provide increasingly-detailed proxy data on paleoenvironments (Section 6).
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653 a Phylogeny
653 a Molecular Genetics
653 a Ecology
653 a Biodiversity
653 a Biogeochemistry
653 a Sedimentation
7001 a Smart, Sandi M.4 aut
7001 a Jentzen, Anna4 aut
7001 a Jonkers, Lukas4 aut
7001 a Morard, Raphaël4 aut
7001 a Meilland, Julie4 aut
7001 a Michel, Elisabeth4 aut
7001 a Coxall, Helen K.u Stockholms universitet,Institutionen för geologiska vetenskaper4 aut0 (Swepub:su)hcoxa
7001 a Hull, Pincelli M.4 aut
7001 a de Garidel-Thoron, Thibault4 aut
7001 a Aze, Tracy4 aut
7001 a Quillévéré, Frédéric4 aut
7001 a Ren, Haojia4 aut
7001 a Sigman, Daniel M.4 aut
7001 a Vonhof, Hubert B.4 aut
7001 a Martinez-García, Alfredo4 aut
7001 a Kučera, Michal4 aut
7001 a Bijma, Jelle4 aut
7001 a Spero, Howard J.4 aut
7001 a Haug, Gerald H.4 aut
7102 a Stockholms universitetb Institutionen för geologiska vetenskaper4 org
7730 t Revue de Micropaleontologied : Elsevier BVg 61:3-4, s. 113-138q 61:3-4<113-138x 0035-1598x 1873-4413
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-163566
8564 8u https://doi.org/10.1016/j.revmic.2018.10.001

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