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Testudines
– from Joyce et al. 2013
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======== $search object ======== Array ( [SimpleSearch] => [FilterByTipTaxa] => Array ( [TaxonA] => [TaxonB] => ) [FilterByClade] => Testudines [FilterByAge] => Array ( [MinAge] => [MaxAge] => ) [FilterByGeologicalTime] => [HiddenFilters] => Array ( [0] => FilterByTipTaxa [1] => FilterByAge [2] => FilterByGeologicalTime ) [BlockedFilters] => Array ( [0] => FilterByTipTaxa ) [SortResultsBy] => DATE_ADDED_DESC [ResponseType] => HTML )
Raising the Standard in Fossil Calibration
The Fossil Calibration Database is a curated collection of well-justified calibrations, including many published in the journal Palaeontologia Electronica. We also promote best practices for justifying fossil calibrations and citing calibrations properly.
CLADE SUBMITTED: Testudines
nameToSourceNodeInfo('Testudines') return this node_data:
Array ( [taxonid] => 8459 [source] => NCBI )
Array ( [taxonid] => 8459 [source] => NCBI )
nameToMultitreeID('Testudines') returns ID:
-1674
-1674
QUERY:
SELECT DISTINCT calibration_id FROM calibrations_by_NCBI_clade WHERE clade_root_multitree_id = '-1674' AND calibration_id IN (SELECT CalibrationID FROM calibrations WHERE PublicationStatus = 4)
SELECT DISTINCT calibration_id FROM calibrations_by_NCBI_clade WHERE clade_root_multitree_id = '-1674' AND calibration_id IN (SELECT CalibrationID FROM calibrations WHERE PublicationStatus = 4)
Adding calibration 244 (inner add-op or non-cladistic search)
'Testudines':
displayedRelevance: 1 / 1 = 1.00
Array ( [CalibrationID] => 244 [NodeName] => Testudines [HigherTaxon] => Reptilia [MinAge] => 155.6 [MinAgeExplanation] => The holotype of <i>Caribemys oxfordiensis</i> de la Fuente and Iturralde-Vinent, 2001 (MNHNCu P-3209) from the Oxfordian Jugua Formation of Cuba is a total group pleurodire and thus placed inside crown Testudines has been universally accepted (e.g., de la Fuente and Iturralde-Vinent, 2001; Gaffney et al., 2006; Joyce, 2007; Sterli and de la Fuente, 2011; Anquetin, 2012). Thus the minimum constraint on the age of crown Testudines is placed at the top of the Oxfordian (155.7 ± 4.0 Ma; Gradstein et al., 2004; Ogg et al., 2008) at 155.6 Ma. [MaxAge] => 251.4 [MaxAgeExplanation] => A constraint for the oldest possible age of the turtle crown must encompass <i>Proterochersis robusta</i>, even though its status as a crown turtle is highly questionable. The Lower to Middle Triassic has produced just one total group testudine, <i>Odontochelys semitestacea</i> Li et al., 2008, and we see no reason to doubt its placement as the oldest unambiguous stem-turtle (Anquetin, 2012). Rich Permian fossil sites worldwide have failed to yield anything that resembles a crown turtle, beyond the enigmatic <i>Eunotosaurus africanus</i> Seeley, 1892, which generally appears to serve the role of an early stem turtle well (Lyson et al., 2010). We therefore place our hard maximum at the base of the Triassic (251.0 ± 0.4 Ma; Gradstein et al., 2004; Ogg et al., 2008) at 251.4 Ma. [PrimaryLinkedFossilID] => 173 [DateCreated] => 2014-10-08 16:19:52 [PublicationID] => 374 [ShortName] => Joyce et al. 2013 [FullReference] => Joyce, W.G., Parham, J.F., Lyson, T.R., Warnock, R.C.M., Donoghue, P.C.J. 2013. A divergence dating analysis of turtles using fossil calibrations: an example of best practices. Journal of Paleontology 87, 612-634. [DOI] => [image] => [image_caption] => [qualifiers] => Array ( [0] => Array ( [relationship] => 07-CLADE-MEMBER [relevance] => 1 ) ) [displayedRelationship] => 07-CLADE-MEMBER [displayedRelevance] => 1.00 )
155.6–251.4 Ma | Added Oct 08, 2014 |
Joyce, W.G., Parham, J.F., Lyson, T.R., Warnock, R.C.M., Donoghue, P.C.J. 2013. A divergence dating analysis of turtles using fossil calibrations: an example of best practices. Journal of Paleontology 87, 612-634.
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