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Reconstructing a dismembered Neogene basin along the active Hikurangi subduction margin, New Zealand
Going round the twist—an empirical analysis of shell coiling in helicospiral gastropods
Spatial scaling of beta diversity in the shallow-marine fossil record
The Pull of the Recent revisited: negligible species-level effect in a regional marine fossil record
Ephemeral species in the fossil record? Synchronous coupling of macroevolutionary dynamics in mid-Paleozoic zooplankton
Completeness of the known graptoloid palaeontological record
Anchors and snorkels: heterochrony, development and form in functionally constrained fossil crassatellid bivalves
Early to middle Eocene magneto-biochronology of the southwest Pacific Ocean and climate influence on sedimentation: Insights from the Mead Stream section, New Zealand
Aragonite bias, and lack of bias, in the fossil record: lithological, environmental, and ecological controls
Identification and independence: morphometrics of Cenozoic New Zealand Spissatella and Eucrassatella (Bivalvia, Crassatellidae)
Graptoloid evolutionary rates track Ordovician–Silurian global climate change
The fossil record and spatial structuring of environments and biodiversity in the Cenozoic of New Zealand
Abstract There is increasing evidence to suggest that drivers of bias in the fossil record have also affected actual biodiversity history, so that controls of artefact and true pattern are confounded. Here we examine the role of spatial structuring of the environment as one component of this common cause hypothesis. Our results are based on sampling standardized analyses of the post-Middle Eocene record of shelf molluscs from New Zealand. We find that spatial structuring of the environment directly influenced the quality of the fossil record. Contrary to our expectations, however, we find no evidence to suggest that spatial structuring of the environment was a strong or direct driver of taxic rates, net diversity, or spatial structuring in mollusc faunas at the scale of analysis. Stage-to-stage variation in sampling standardized diversity over the past 40 Ma exhibits two superficially independent dynamics: (a) changes in net diversity were associated primarily with changes in origination rate; and (b) an unknown common cause related extinction rate to the quality of the fossil record and, indirectly, to spatial structuring of the environment. We suggest that tectonic drivers, manifest as second-order sequence stratigraphic cycles, are likely to have been a key element of this common cause.