A case for subgenera in a foraminiferal classification

There has been a progression in palaeobiological classifications from the more primitive empirical “stamp collecting” stage where similar shapes were grouped together, to the more sophisticated phylogenetic classifications where supposed genetically related foraminiferal taxa are categorised togethe...

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Published in:Journal of Micropalaeontology
Main Author: Jenkins, D. Graham
Format: Article in Journal/Newspaper
Language:English
Published: GSL Publishing 1990
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Online Access:https://doi.org/10.1144/jm.9.1.36
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00038391 2023-05-15T18:00:59+02:00 A case for subgenera in a foraminiferal classification Jenkins, D. Graham 1990-07 electronic https://doi.org/10.1144/jm.9.1.36 https://noa.gwlb.de/receive/cop_mods_00038391 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00038069/jm-9-36-1990.pdf https://jm.copernicus.org/articles/9/36/1990/jm-9-36-1990.pdf eng eng GSL Publishing Journal of Micropalaeontology -- http://www.bibliothek.uni-regensburg.de/ezeit/?2053393 -- https://www.j-micropalaeontol.net/volumes.html -- http://jm.geoscienceworld.org/ -- 2041-4978 https://doi.org/10.1144/jm.9.1.36 https://noa.gwlb.de/receive/cop_mods_00038391 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00038069/jm-9-36-1990.pdf https://jm.copernicus.org/articles/9/36/1990/jm-9-36-1990.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 1990 ftnonlinearchiv https://doi.org/10.1144/jm.9.1.36 2022-02-08T22:43:06Z There has been a progression in palaeobiological classifications from the more primitive empirical “stamp collecting” stage where similar shapes were grouped together, to the more sophisticated phylogenetic classifications where supposed genetically related foraminiferal taxa are categorised together. But how do we know that certain extinct taxa were genetically related? This is a major problem where a number of factors interplay together: a belief in evolution, the experience of the operator and consequent recognition of phyletic lineages. In the study of Cenozoic planktonic foraminifera we are fortunate to have recognised a number of now well established lineages; also we have some data on amino-acids found in the tests of living species (King and Hare, 1972) which range back well into the Neogene. These latter data not only provide us with essential genetic information but they also give us confidence when dealing with the classification of extinct species. So how do we build this evolutionary knowledge into a classification? Clearly, genetically related species can be grouped together into subgenera, and related subgenera into broader genera. In their classification Loeblich and Tappan (1988) held a different view and decided not to use subgenera because (1) their usage produces an unwieldy classification, and (2) lineage concepts change when additional data are collected. If we follow their classification, then when you read about Globorotalia menardii, Globorotalia fohsi and Globorotalia hirsuta you could assume that they are closely related; this is not true. The three species have similar test morphologies but these have resulted from iterative. . . Article in Journal/Newspaper Planktonic foraminifera Niedersächsisches Online-Archiv NOA Journal of Micropalaeontology 9 1 36 36
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language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Jenkins, D. Graham
A case for subgenera in a foraminiferal classification
topic_facet article
Verlagsveröffentlichung
description There has been a progression in palaeobiological classifications from the more primitive empirical “stamp collecting” stage where similar shapes were grouped together, to the more sophisticated phylogenetic classifications where supposed genetically related foraminiferal taxa are categorised together. But how do we know that certain extinct taxa were genetically related? This is a major problem where a number of factors interplay together: a belief in evolution, the experience of the operator and consequent recognition of phyletic lineages. In the study of Cenozoic planktonic foraminifera we are fortunate to have recognised a number of now well established lineages; also we have some data on amino-acids found in the tests of living species (King and Hare, 1972) which range back well into the Neogene. These latter data not only provide us with essential genetic information but they also give us confidence when dealing with the classification of extinct species. So how do we build this evolutionary knowledge into a classification? Clearly, genetically related species can be grouped together into subgenera, and related subgenera into broader genera. In their classification Loeblich and Tappan (1988) held a different view and decided not to use subgenera because (1) their usage produces an unwieldy classification, and (2) lineage concepts change when additional data are collected. If we follow their classification, then when you read about Globorotalia menardii, Globorotalia fohsi and Globorotalia hirsuta you could assume that they are closely related; this is not true. The three species have similar test morphologies but these have resulted from iterative. . .
format Article in Journal/Newspaper
author Jenkins, D. Graham
author_facet Jenkins, D. Graham
author_sort Jenkins, D. Graham
title A case for subgenera in a foraminiferal classification
title_short A case for subgenera in a foraminiferal classification
title_full A case for subgenera in a foraminiferal classification
title_fullStr A case for subgenera in a foraminiferal classification
title_full_unstemmed A case for subgenera in a foraminiferal classification
title_sort case for subgenera in a foraminiferal classification
publisher GSL Publishing
publishDate 1990
url https://doi.org/10.1144/jm.9.1.36
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https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00038069/jm-9-36-1990.pdf
https://jm.copernicus.org/articles/9/36/1990/jm-9-36-1990.pdf
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation Journal of Micropalaeontology -- http://www.bibliothek.uni-regensburg.de/ezeit/?2053393 -- https://www.j-micropalaeontol.net/volumes.html -- http://jm.geoscienceworld.org/ -- 2041-4978
https://doi.org/10.1144/jm.9.1.36
https://noa.gwlb.de/receive/cop_mods_00038391
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00038069/jm-9-36-1990.pdf
https://jm.copernicus.org/articles/9/36/1990/jm-9-36-1990.pdf
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container_title Journal of Micropalaeontology
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