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Monday, September 16, 2019

Lake Ohrid drill cores reveal 1.36 million years of European climate history

Lake Ohrid, at the border 
between Albania and 
North Macedonia, is the 
oldest existing lake 
in Europe.









The ICDP Drilling Program 
in Lake Ohrid was funded 
by the German Research 
Foundation (DFG), the 
German Federal Ministry 
of Education and Research, 
the University of Cologne 
and other international donors.

The deep drilling 
was done in 2013. 

The maximum drilling depth 
was 568 meters, below a
water depth of 245 meters.

Analysis of the extracted
drill cores, with their 
sediment layers, 
took five years.

The Lake Ohrid project 
involved 47 researchers 
from 13 nations.

The team was headed by 
the geologist Professor 
Bernd Wagner from the 
University of Cologne.

They published 
some findings, titled:
"Mediterranean winter rainfall 
in phase with African monsoon 
during past 1.36 million years"
in 'Nature'.

"We have shown that the 
lake formed exactly 
1.36 million years ago 
and has existed 
continuously ever since", 
geologists Dr Bernd Wagner 
and Dr Hendrik Vogel 
(University of Bern) said. 

"We were thrilled 
when we realized 
that we had retrieved 
one of the longest 
and most complete 
lake sediment cores 
from the oldest lake 
in Europe."

"Getting the chance 
to obtain high-resolution 
regional climate data 
for a period of over 
1.3 million years
is the dream of every 
climate researcher."

The sediments 
allow scientists 
to reconstruct
the climate history 
of the region.

This can now 
be compared with 
estimates from models.

The sediment data show 
a significant increase 
in winter precipitation 
in the northern 
Mediterranean region 
during the warm seasons. 

The Mediterranean climate
is characterized by strong 
seasonal contrasts 
between dry summers 
and wet winters. 

Changes in winter rainfall 
had been difficult 
to reconstruct on 
time scales of the 
last million years.

Because there are
so few regional 
hydro-climate records 
covering several 
glacial-interglacial cycles 
with different earth 
orbital geometries, 
global ice volume 
and atmospheric 
greenhouse gas 
concentrations.