Adrian Paterson

Adrian Paterson

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Research Focus & Metrics

Academic Career Length

34Years (1993-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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9 January 2008 in Geological Magazine
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CLC. A. Landis
C. A. Landis
HCH. J. Campbell
H. J. Campbell
JBJ. G. Begg
J. G. Begg
DMD. C. Mildenhall
D. C. Mildenhall
APAdrian Paterson
Adrian Paterson
Steven TrewickSteven Trewick
Steven Trewick
The Waipounamu Erosion Surface is a time-transgressive, nearly planar, wave-cut surface. It is not a peneplain. Formation of the Waipounamu Erosion Surface began in Late Cretaceous time following break-up of Gondwanaland, and continued until earliest Miocene time, during a 60 million year period of widespread tectonic quiescence, thermal subsidence and marine transgression. Sedimentary facies and geomorphological evidence suggest that the erosion surface may have eventually covered the New Zealand subcontinent (Zealandia). We can find no geological evidence to indicate that land areas were continuously present throughout the middle Cenozoic. Important implications of this conclusion are: (1) the New Zealand subcontinent was largely, or entirely, submerged and (2) New Zealand's present terrestrial fauna and flora evolved largely from fortuitous arrivals during the past 22 million years. Thus the modern terrestrial biota may not be descended from archaic ancestors residing on Zealandia when it broke away from Gondwanaland in the Cretaceous, since the terrestrial biota would have been extinguished if this landmass was submerged in Oligocene–Early Miocene time. We conclude that there is insufficient geological basis for assuming that land was continuously present in the New Zealand region through Oligocene to Early Miocene time, and we therefore contemplate the alternative possibility, complete submergence of Zealandia.

13 December 2006 in Journal of Biogeography
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Steven TrewickSteven Trewick
Steven Trewick
APAdrian Paterson
Adrian Paterson
HCHamish J. Campbell
Hamish J. Campbell

15 March 2010 in Ecology Letters
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CMCatriona J. MacLeod
Catriona J. MacLeod
APAdrian Paterson
Adrian Paterson
DTDaniel M. Tompkins
Daniel M. Tompkins
RDRichard P. Duncan
Richard P. Duncan

1 July 2001 in International Journal for Parasitology
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Journal Article
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APAdrian Paterson
Adrian Paterson
JBJonathan Banks
Jonathan Banks

4 September 2008 in Philosophical Transactions of the Royal Society B: Biological Sciences
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JGJulia Goldberg
Julia Goldberg
Steven TrewickSteven Trewick
Steven Trewick
APAdrian Paterson
Adrian Paterson
New Zealand biogeography has been dominated by the knowledge that its geophysical history is continental in nature. The continental crust (Zealandia) from which New Zealand is formed broke from Gondwanaland ca 80 Ma, and there has existed a pervading view that the native biota is primarily a product of this long isolation. However, molecular studies of terrestrial animals and plants in New Zealand indicate that many taxa arrived since isolation of the land, and that diversification in most groups is relatively recent. This is consistent with evidence for species turnover from the fossil record, taxonomic affinity, tectonic evidence and observations of biological composition and interactions. Extinction, colonization and speciation have yielded a biota in New Zealand which is, in most respects, more like that of an oceanic archipelago than a continent.

28 October 2009 in Wildlife Research
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SMS. A. Morgan
S. A. Morgan
CHC. M. Hansen
C. M. Hansen
JRJames Ross
James Ross
GHG. J. Hickling
G. J. Hickling
SOShaun Ogilvie
Shaun Ogilvie
APAdrian Paterson
Adrian Paterson
Context. House cats are increasingly suggested as having major ecological impacts in semiurban environments. Information on the activity of house cats is relatively scarce, especially in habitats such as wetlands. Aims. This study examines the movement and foraging behaviour of house cats living on the periphery of a wetland reserve in Christchurch city, New Zealand. Methods. Twenty-one domestic cats living in a suburban residential area were studied using radiotelemetry to determine home-range size, mean and maximum distances travelled into the adjacent wetland, and the proportion of time spent in the wetland over a 12-month period. Surveys of prey retrieval for 88 cats were also carried out by cat owners over the same 12-month period. Key results. Cat age and the distance of the cat’s home from the periphery of the wetland were highly correlated with cat movement and hunting activity. These movements were not markedly influenced by season or time of day. Younger cats (<6 years of age) living on the periphery of the wetland had larger home-range sizes, moved significantly further into the wetland and spent a significantly greater proportion of time in the wetland. Cats living close to the wetland also brought a greater diversity and a greater total number of prey items to their home-site. Rates of predation were not significantly influenced by sex or whether the cat was wearing a bell. The most common prey items were introduced rodents and birds; however, 172 of 981 prey items were identified as a native common skink. Conclusions.Consequently, cats living in households on the wetland periphery currently pose a predation risk for the wetland species, and the impact of cats on the native skink population warrants further investigation. Implications. This study suggests that domestic cats will exploit wild habitats but that their potential impact will have both positive (predation of introduced pest species) and negative (occasional direct predation) effects on native wildlife.