(1) 40Ar39Ar dating and isotopic geochemistry
of large igneous provinces.
Not exact matches
One suspect behind several mass extinctions is a kind
of enormous volcanic zone called a
large igneous province, or LIP.
Large igneous provinces, or LIPs, are huge pools
of volcanic rocks poured out at the Earth's surface.
Eventually the magma ran out, leaving a
large igneous province — a 20 - mile - thick pile
of volcanic rocks.
Their findings further substantiate the critical role
of mantle plumes in forming
large igneous provinces.
High - precision dating
of the Kalkarindji
large igneous province, Australia, and synchrony with the Early — Middle Cambrian (Stage 4 — 5) extinction
In Earth's past the trigger for these greenhouse gas emissions was often unusually massive volcanic eruptions known as «
Large Igneous Provinces,» with knock - on effects that included huge releases
of CO2 and methane from organic - rich sediments.
Proposed hypothe - ses include (i) biogenic methane from gas hydrate dissociation (Dickens et al., 1995,1997); (ii) CO2 from extensive oxidation terrestrial organic carbon (Kurtz et al., 2003; Deconto et al., 2012); (iii) thermogenic methane derived from emplacement
of a
large 25
igneous province (LIP) in the North Atlantic (Svensen et al., 2010) or combinations
of such sources (Sluijs et al., 2007; Panchuk et al., 2008).
While the biggest volcanic eruptions — including
large igneous provinces like the Siberian Traps — are known to be linked to climate upheaval and even mass extinctions, emerging work shows that under the right conditions, smaller eruptions or series
of eruptions can also affect climate.