Akatore Study Published in Earth and Planetary
Earth and Planetary Science Letters 520 (2019) 18–25 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Kelp DNA records late Holocene paleoseismic uplift of coastline, southeastern New Zealand ∗ Elahe Parvizi a, Dave Craw b, , Jonathan M. Waters a a Zoology Department, University of Otago, PO Box 56, Dunedin 9054, New Zealand b Geology Department, University of Otago, PO Box 56, Dunedin 9054, New Zealand a r t i c l e i n f o a b s t r a c t Article history: Holocene paleoseismic activity on the Akatore Fault zone, southeastern New Zealand, has caused uplift Received 20 January 2019 of a 23 km section of coastline by several metres. Prominent relict shoreline terraces are preserved at Received in revised form 4 May 2019 6 m and 3 m above the present sea level, and the latter terrace was formed 1000-1400 yrs BP. The Accepted 22 May 2019 main fault strand farther inland has 6 mof late Holocene vertical offset, but the relationships between Available online xxxx coastal offsets and fault offsets are not understood. There is no preserved geological evidence on the Editor: J.-P. Avouac coastline to distinguish between incremental uplift (e.g., numerous centimetre-scale events) and major, Keywords: metre-scale, uplift events: a distinction that is important for evaluating regional paleoseismicity. We have paleoseismology used genetic characterisation of populations of live kelp, Durvillaea antarctica growing along the shoreline neotectonics to investigate whether or not there has been a catastrophic uplift event, greater than the two metre tidal fault range, that was sufficient to extirpate intertidal kelp populations.
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