One
explanation for dinosaur extinction around the Cretaceous-Tertiary
boundary 65 million years ago implicates a volcanic eruption in India
whose dust and CO2 emissions altered
atmospheric chemistry and climate.
CNRS
researchers from the "Laboratoire de Mécanismes de Transfert
en Géologie" (LMTG, Geological Transfer Mechanisms Laboratory)
in collaboration with the "Institut de Physique du Globe de Paris"(Paris
Geophysical Institute) and the "Laboratoire de Physique Atmosphérique
et Planétaire de Liège" (Laboratory for Planetary
and Atmospheric Physics of the University of Liège) used a
numerical model to show that thick basalt lavas, the Deccan Traps,
copiously deposited in northwest India at that time, caused such changes.
Results indicate that for over one million years, a balance was regulated
by a source and sink system, respectively volcanic outgassing and
silicate chemical weathering, acting as a CO2-consuming
pump.
Basalts
are the silicate rocks most susceptible to weathering and the Deccan
Traps have shrunk by two-thirds in 65 million years. Researchers derived
a law for CO2 consumption in basalt
weathering from data taken from rivers draining the Deccan Traps and
other basaltic regions. Runoff and atmospheric temperature were the
main factors controlling soil and rock
solubility and hence CO2 consumption
rate.
The
model predicted oceanic carbon and strontium cycle variations. The
emplacement of the Deccan Traps was responsible for a strong increase
of atmospheric CO2 by 1050 ppmv (triple
the present rate) and a global temperature increase of 4°C. Subsequent
continental weathering over 1.5 million years was enough for excess
atmospheric to be reabsorbed, with consequent global cooling of 0.55
°C. Moreover, this important CO2 outgassing caused a sharp decrease
in carbonate sedimentation (-45% in only 20,000 years) via a strong
sea-water acidification.
This pause is observed in marine carbonates at the Cretaceous/Tertiary
boundary.
This CO2 peak and global warming
support the idea that, whatever caused dinosaur extinction, volcanic
eruption and the formation of the Deccan Traps greatly amplified that
crisis.