Australasian Science 11-1

(Chris Devlin) #1

10 | JAN/FEB 2016


CSIRO has developed an innovative coating
for medical devices and implants made from
prebiotic “goo” that can be traced back
billions of years to the origin of life.
Dr Richard Evans of CSIRO said
hundreds of thousands of Australians

receive medical implants like bone replace-
ments, catheters and pacemakers every year.
“Reducing the likelihood of infection, and
ensuring the body doesn’t reject implants,
are ongoing medical challenges,” he said.
“That’s why coatings on these implants are

needed to help them to do their job.
“We wanted to use these prehistoric
molecules, which are believed to have been
the source of all life evolving on Earth, to see
if we could apply the chemistry in a practical
way.”
The team discovered that the nitroge-
nous polymer aminomalononitrile is bio-
friendly, and cells readily grow and colonise
it. “The non-toxic coating is adhesive and
will coat almost any material, making its
potential biomedical applications really
broad,” Evans said.
The researchers also tried adding silver
compounds to produce an antibacterial
coating that can be used on devices such as
catheters to avoid infections. “Other
compounds can also be added to implants
to reduce friction, make them more durable
and resistant to wear,” Evans said.
The coating process is very simple and
uses methods and substances that are readily
available, making devices more cost-effective
for biomedical manufacturers.
The findings from the research were
published inAsia Materials(tinyurl.com/
nqmhylb).

Primordial Goo Improves Implants


f

p
n

Dr Richard Evans has developed a
bio-friendly coating for medical implants
that improves their performance and
acceptance by the body.

Microplate Discovery Dates
Birth of Himalayas
The discovery of the first oceanic microplate in the Indian Ocean
is helping an international team of scientists to identify when the
initial collision between India and Eurasia led to the birth of the
Himalayas.
At least seven microplates are known in the Pacific Ocean, but
this is the first ancient Indian Ocean microplate discovered. Radar
beam images from an orbiting satellite have helped put together
pieces of this plate tectonic jigsaw and pinpointed the age for the
collision, whose precise date has divided scientists for decades.
Reported in Earth and Planetary Science Letters(tinyurl.com/
onutrlv), the team believes the collision occurred 47 million years
ago when India and Eurasia initially smashed into each other.
“The age of the largest continental collision on Earth has long been
controversial, with age estimates ranging from at least 59 to 34
million years ago,” said lead author Dr Kara Matthews of The Univer-
sity of Sydney. “Knowing this age is particularly important for under-
standing the link between the growth of mountain belts and major
climate change.”
The researchers discovered that crustal stresses caused by the
initial collision cracked the Antarctic Plate far away from the colli-
sional zone and broke off a fragment the size of Tasmania in a
remote patch of the central Indian Ocean. The authors have named
this the Mammerickx Microplate after Dr Jacqueline Mammerickx,
a pioneer in seafloor mapping.
Rotation of the Mammerickx Microplate is revealed by a rotating
pattern of grooves and hills that turn the topography of the ocean

floor into a jagged landscape. These “abyssal hills” record a sudden
increase in crustal stress that date the birth of the Himalayan
mountains to 47 million years ago.
The new research shows that 50 million years ago, India was trav-
elling northwards at speeds of 15 cm/year. Soon after it slammed
into Eurasia, crustal stresses along the mid-ocean ridge between
India and Antarctica intensified to breaking point. A chunk of
Antarctica’s crust broke off and started rotating like a ball bearing,
creating the Mammerickx Microplate.
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