International researchers discover development of ocean currents
The Gulf Stream transports ocean heat across the Atlantic towards the
northeast and this gives rise to thriving palm trees in Ireland and
allows ports to remain ice-free during the winter. Likewise, most ocean
currents have a large impact on the global climate. Since when did this
system work the way we know it today? And how did it develop?
Ocean currents play a major factor in our climate. The Gulf Stream
transports so much heat from the tropical Atlantic towards the
northeast that the winters in northern Europe are relatively mild and
humid in relation to other regions at similar latitudes. This transport
of heat simultaneously causes a cooling down in the South Atlantic, a
process known as heat piracy.
However, the pattern of today's global
ocean currents is relatively recent, having developed during the
Pliocene era, a mere six to two and a half million years ago.
The movement of tectonic plates has an impact on the opening and
closing of straits / channels. The extent to which the present-day heat
piracy in the North Atlantic has evolved in the face of tectonic
changes is insufficiently understood.
An international team of
paleo-oceanographers, with the collaboration of GEOMAR, has published
their findings about the process in a recent issue of the Scientific
Deep sea drilling in the North and South Atlantic formed the foundation
for the new findings, in the form of core samples taken from the
seabed. Fossils of single-celled microorganisms (foraminifera) have
been found in these cores.
According to first author Dr Cyrus Karas
from Lamont-Doherty Earth Observatory in the US, if the isotopes and
trace metals in the foraminifera were measured, the data would allow
them to reconstruct the physical conditions of oceans in the past (such
as oceanic temperatures) very accurately.
“The Pliocene in fact is an epoch in Earth history, which is characterised by extremely dynamic plate-tectonic movements,” said co-author Dirk Nuernberg from GEOMAR.
study shows that the tectonic changes in the Strait of Gibraltar in the
Mediterranean, the formation of the Central American land bridge, and
the constriction of the Indonesian Seaway have had immense subsequent
impacts on the global oceanic overturning circulation over time, and
thus on the temperatures in the North and South Atlantic”.
A change in the Mediterranean throughflow about 5.3 million years ago
weakened the Atlantic Overturning Circulation, leading to a warming of
the South Atlantic in relation to the North Atlantic. Then, between 4.8
and 3.8 million years ago, the oceanic connection between the Atlantic
and Pacific narrowed.
When the Central American landbridge was formed,
this connection closed. This process intensified the Gulf Stream,
causing the North Atlantic to warm by circa two degrees Celsius at the
expense of the South Atlantic – expressing active heat piracy that
lasts to this day.
With the tectonic constriction of the Indonesian sea route 3.8 to three
million years ago, a weakening of the global recirculation circulation
could be detected from the geochemical data, which is related to the
start of glaciations of the Northern Hemisphere.
importance of our paleoceanographic study is to provide evidence of how
local tectonic changes have radically altered the ocean temperatures in
the North and South Atlantic and thus, effectively influenced global
climate,” said Dr Karas.