Step 1: Recall major mass extinction events.
- Cretaceous–Paleogene (K–Pg, 66 Ma): Caused by asteroid impact and volcanism (Deccan traps).
- Permian–Triassic (252 Ma): Largest extinction, linked to Siberian Traps volcanism, ocean anoxia, methane release.
- Ordovician–Silurian (445 Ma): Caused mainly by global cooling, Gondwana glaciation, and associated sea-level fall. This event wiped out more than 50% of marine fauna.
- Holocene (ongoing): Linked to human activities, not glaciation.
Step 2: Identify correct extinction.
Only the Ordovician–Silurian event was directly caused by global cooling, glaciation, and sea-level fall.
Final Answer:
\[
\boxed{\text{Ordovician – Silurian}}
\]
While doing Bayesian inference, consider estimating the posterior distribution of the model parameter (m), given data (d). Assume that Prior and Likelihood are proportional to Gaussian functions given by \[ {Prior} \propto \exp(-0.5(m - 1)^2) \] \[ {Likelihood} \propto \exp(-0.5(m - 3)^2) \] 
The mean of the posterior distribution is (Answer in integer)
Consider a medium of uniform resistivity with a pair of source and sink electrodes separated by a distance \( L \), as shown in the figure. The fraction of the input current \( (I) \) that flows horizontally \( (I_x) \) across the median plane between depths \( z_1 = \frac{L}{2} \) and \( z_2 = \frac{L\sqrt{3}}{2} \), is given by \( \frac{I_x}{I} = \frac{L}{\pi} \int_{z_1}^{z_2} \frac{dz}{(L^2/4 + z^2)} \). The value of \( \frac{I_x}{I} \) is equal to 
Suppose a mountain at location A is in isostatic equilibrium with a column at location B, which is at sea-level, as shown in the figure. The height of the mountain is 4 km and the thickness of the crust at B is 1 km. Given that the densities of crust and mantle are 2700 kg/m\(^3\) and 3300 kg/m\(^3\), respectively, the thickness of the mountain root (r1) is km. (Answer in integer)