With a little kelp from my friends

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New Zealand
Photo by Ben Wicks on Unsplash
Photo by Ben Wicks on Unsplash

Rocky coastal areas disturbed by earthquakes can be recolonised by genetically different kelp drifting from hundreds of kilometres away - meaning that kelp has the potential to record geological events. By combining laser mapping data and kelp genetics researchers identified a previously unknown area of earthquake uplift in Marlborough, where a raised area 1 metre above sea level had a genetic anomaly in kelp below that area. The authors say this work shows that earthquake uplift leaves long lasting signatures in New Zealand's coastal species, and also highlights the new discoveries possible when disciplines such as geology and genetics are combined.

Media release

From: University of Otago

Otago researchers reveal impact of ancient earthquake

By combining the scientific powerhouses of genetics and geology, University of Otago researchers
have identified a new area of coastal uplift, which had been hiding in plain sight.


The previously unknown region of earthquake uplift, in Rarangi, Marlborough, was discovered using
a combination of new data from laser mapping and kelp genetics.


Co-author Professor Jon Waters, of the Department of Zoology, says the study gives new insights
into the changes in Aotearoa’s landscapes and the recent history of earthquake impacts.


“In a geologically well studied country like New Zealand, there is still a lot to learn about our history
of earthquakes and changing landforms,” he says.

The paper, just published in Journal of the Royal Society Interface, utilised LiDAR mapping (remote
sensing technology used to model ground elevation) and genetic analysis of bull kelp from the
uplifted section of coast.


The team identified a previously unrecognised area of uplifted rocky coastline – a bench about 1m
above sea level – and a genetic anomaly in kelp below that bench. The kelp’s genetics indicate the
species went extinct in the area following an earthquake, before being recolonised by kelp which
drifted from 300km south.


The group believe the earthquake responsible occurred about 2000 to 3000 years ago, showing the
potential for kelp to record geological disturbance events.


“The area is close to a well-known active fault and several big, past earthquakes have been well
quantified by other researchers, but this coastal uplift zone was not previously known – the evidence
for it is extremely clear now we’ve had a chance to look more closely.


“Rarangi is also a very popular summer swimming spot, rather than some obscure or remote
location, and the evidence of coastal uplift was hiding in plain sight,” Professor Waters says. 
The research is the latest output from the group’s Marsden-funded project assessing earthquake
impacts on coastal species.


“Our work uses a combination of genetics and geology, and it’s quite exciting that these combined
approaches have allowed us to pinpoint a previously unknown site of coastal uplift in New Zealand.
“This work serves to highlight again just how dynamic our country is – and how earthquake uplift
leaves long lasting signatures in our coastal species.”

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Research The Royal Society, Web page The URL will go live after the embargo ends.
Journal/
conference:
Journal of the Royal Society Interface
Research:Paper
Organisation/s: University of Otago
Funder: This work was supported by the Marsden Fund administered by Royal Society of New Zealand Te Apārangi, contract 18-UOO-172. C.I.F. was supported by a Rutherford Discovery Fellowship from the Royal Society of New Zealand Te Apārangi (grant no. RDFUOO1803).
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