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- W1973667524 endingPage "47" @default.
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- W1973667524 abstract "Abstract Evolution occurred equally through allopatric speciation and anagenesis during Pliocene–Early Pleistocene time. However, no anagenesis is observed in Castlecliffian to Recent Mollusca. Possible explanations include (1) increasing shallowness and energy of the environment (Sheldon's ‘plus ça change’ model); (2) lecithotrophs increased with falling temperatures, and are more susceptible than planktotrophs to allopatric speciation; (3) ‘plus ça change’ implies that anagenesis continued unabated, but unrecorded, offshore from the recorded Pleistocene fauna. Three lineages (Pelicaria vermis, Stiracolpus symmetricus, Aoteadrillia wanganuiensis) became highly variable as a result of their changed developmental mode. Origination continued throughout Castlecliffian–Haweran time at a background rate of 0–2 new species per oxygen isotope stage (OIS), whereas extinction and range extensions of warm-water taxa to Wanganui Basin both reached a peak in OIS 9–7. However, the faunal record results from the interplay of temperature change and the preservation of different depositional environments. Biostratigraphy and temperature change also are reviewed." @default.
- W1973667524 created "2016-06-24" @default.
- W1973667524 creator A5041370586 @default.
- W1973667524 date "2012-02-24" @default.
- W1973667524 modified "2023-09-27" @default.
- W1973667524 title "Marine Mollusca of the last 2 million years in New Zealand. Part 5. Summary" @default.
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