Matches in SemOpenAlex for { <https://semopenalex.org/work/W2005868711> ?p ?o ?g. }
- W2005868711 endingPage "41" @default.
- W2005868711 startingPage "18" @default.
- W2005868711 abstract "Abstract The first half of tetrapod evolution witnessed substantial diversification of the clade and several major turnovers and mass extinctions. In the time since their origin, more than 380 Myr ago, to the beginning of the Middle Jurassic 175 Myr ago, tetrapods apparently diversified fitfully, reaching their highest level in the Middle Permian, and showing major diversity declines in the late Moscovian, Early Permian, Wordian, lower Wuchiapingian, end-Permian, lower Anisian, lower Ladinian, Late Triassic (lower Norian to upper Rhaetian), end-Triassic, and Early Jurassic (upper Sinemurian, lower Pliensbachian). Of these diversity drops, only the end-Permian and end-Triassic correspond to recognised mass extinctions, and the late Moscovian and early Norian drops to other previously identified environmental crises. The remainder could be real extinction or turnover events, or partially artefacts of biased sampling. There are strong correlations between formation counts and tetrapod palaeodiversity, suggesting a sampling component in the raw data, but the covariation is not uniform through the whole time span, being poor from Devonian to Middle Permian, and better from Late Permian to Early Jurassic. There is limited evidence for covariation between the tetrapod palaeodiversity time series and other putative sampling metrics, such as specimen completeness, numbers of publications, map areas, gap-bounded sedimentary units, rock volumes, formations, and fossil collections. Modelling by multiple correlations shows that formation count is generally the best explanatory model, either on its own, or combined with other ‘sampling’ time series. However, it is not clear that formation count is independent of the palaeodiversity time series, because rises and falls in both signals could reflect variations in original diversity or in preservation or in sampling." @default.
- W2005868711 created "2016-06-24" @default.
- W2005868711 creator A5025071876 @default.
- W2005868711 creator A5029744192 @default.
- W2005868711 creator A5031264398 @default.
- W2005868711 creator A5085772875 @default.
- W2005868711 date "2013-02-01" @default.
- W2005868711 modified "2023-10-01" @default.
- W2005868711 title "The first half of tetrapod evolution, sampling proxies, and fossil record quality" @default.
- W2005868711 cites W1546559141 @default.
- W2005868711 cites W1553148337 @default.
- W2005868711 cites W1968883957 @default.
- W2005868711 cites W1969715735 @default.
- W2005868711 cites W1970741654 @default.
- W2005868711 cites W1974446702 @default.
- W2005868711 cites W1975276945 @default.
- W2005868711 cites W1976725247 @default.
- W2005868711 cites W1978097234 @default.
- W2005868711 cites W1978464139 @default.
- W2005868711 cites W1980420809 @default.
- W2005868711 cites W1985298101 @default.
- W2005868711 cites W1986422852 @default.
- W2005868711 cites W1987551148 @default.
- W2005868711 cites W1993570908 @default.
- W2005868711 cites W1999944478 @default.
- W2005868711 cites W2002352667 @default.
- W2005868711 cites W2005571584 @default.
- W2005868711 cites W2009772623 @default.
- W2005868711 cites W2010154591 @default.
- W2005868711 cites W2010722293 @default.
- W2005868711 cites W2017260351 @default.
- W2005868711 cites W2019736558 @default.
- W2005868711 cites W2020042837 @default.
- W2005868711 cites W2020097579 @default.
- W2005868711 cites W2022294619 @default.
- W2005868711 cites W2026768415 @default.
- W2005868711 cites W2030637789 @default.
- W2005868711 cites W2034543157 @default.
- W2005868711 cites W2039651811 @default.
- W2005868711 cites W2042835760 @default.
- W2005868711 cites W2044435308 @default.
- W2005868711 cites W2046619981 @default.
- W2005868711 cites W2047752583 @default.
- W2005868711 cites W2049772270 @default.
- W2005868711 cites W2055826021 @default.
- W2005868711 cites W2057108646 @default.
- W2005868711 cites W2057937776 @default.
- W2005868711 cites W2067999823 @default.
- W2005868711 cites W2087440539 @default.
- W2005868711 cites W2088558337 @default.
- W2005868711 cites W2092302011 @default.
- W2005868711 cites W2094244806 @default.
- W2005868711 cites W2096415445 @default.
- W2005868711 cites W2107644132 @default.
- W2005868711 cites W2110009186 @default.
- W2005868711 cites W2114673435 @default.
- W2005868711 cites W2117504072 @default.
- W2005868711 cites W2117574038 @default.
- W2005868711 cites W2117693226 @default.
- W2005868711 cites W2120110582 @default.
- W2005868711 cites W2122289512 @default.
- W2005868711 cites W2122397575 @default.
- W2005868711 cites W2124823872 @default.
- W2005868711 cites W2125956055 @default.
- W2005868711 cites W2126310917 @default.
- W2005868711 cites W2126398656 @default.
- W2005868711 cites W2130869324 @default.
- W2005868711 cites W2131872692 @default.
- W2005868711 cites W2134481329 @default.
- W2005868711 cites W2136618774 @default.
- W2005868711 cites W2137415783 @default.
- W2005868711 cites W2138701738 @default.
- W2005868711 cites W2140343582 @default.
- W2005868711 cites W2140595946 @default.
- W2005868711 cites W2141169953 @default.
- W2005868711 cites W2148919921 @default.
- W2005868711 cites W2148963181 @default.
- W2005868711 cites W2153512785 @default.
- W2005868711 cites W2156931413 @default.
- W2005868711 cites W2157076521 @default.
- W2005868711 cites W2160118267 @default.
- W2005868711 cites W2160525739 @default.
- W2005868711 cites W2164497055 @default.
- W2005868711 cites W2167917951 @default.
- W2005868711 cites W2169773463 @default.
- W2005868711 cites W2170731154 @default.
- W2005868711 cites W2174571031 @default.
- W2005868711 cites W2175501157 @default.
- W2005868711 cites W2178775884 @default.
- W2005868711 cites W2302143698 @default.
- W2005868711 cites W2315019200 @default.
- W2005868711 cites W2322512228 @default.
- W2005868711 cites W2328366459 @default.
- W2005868711 cites W2413592034 @default.
- W2005868711 cites W2467392096 @default.
- W2005868711 cites W2501786537 @default.
- W2005868711 doi "https://doi.org/10.1016/j.palaeo.2012.09.005" @default.
- W2005868711 hasPublicationYear "2013" @default.