Questions 31-39
: `' }4 c, f0 g9 q! {Perhaps one of the most dramatic and important changes that took place in the
9 K6 P e" c4 l! W( @- t! iMesozoic era occurred late in that era, among the small organisms that populate the
: @& B$ \4 q Q; f& U% G# v: @/ uuppermost, sunlit portion of the oceans--the plankton. The term "plankton" is a broad8 F5 A% {& M3 j# U* @
Line one, designating all of the small plants and animals that float about or weakly propel: X/ P1 ~4 C" c( v) e/ l
(5) themselves through the sea. In the late stages of the Mesozoic era. during the Cretaceous8 F8 `, \0 n: [; f3 u
period, there was a great expansion of plankton that precipitated skeletons or shells
9 N+ n: z, R2 zcomposed of two types of mineral: silica and calcium carbonate. This development
# m0 y7 N, K# P/ Iradically changed the types of sediments that accumulated on the seafloor, because,
9 [7 b7 G0 ?9 u, Jwhile the organic parts of the plankton decayed after the organisms died, their mineralized1 a$ b0 h2 o$ E1 Z% _
(10) skeletons often survived and sank to the bottom. For the first time in the Earth's long. r5 x# r" T3 P3 T& h8 Z d. Z# Y. D
history, very large quantities of silica skeletons, which would eventually harden into rock,
* d( B; e& X f" b Rbegan to pile up in parts of the deep sea. Thick deposits of calcareous ooze made up of
1 y9 G# n( x: ithe tiny remains of the calcium carbonate-secreting plankton also accumulated as never' H5 {' U+ ^ K; L9 H7 {% j V) E
before. The famous white chalk cliffs of Dover, in the southeast of England, are just one
/ Z: {0 e5 ]/ v: Q' B' u(15) example of the huge quantities of such material that amassed during the Cretaceous8 Z) x: I+ }. M8 B0 I9 S
period; there are many more. Just why the calcareous plankton were so prolific during
( V3 B4 l' W H2 A0 U7 ?the latter part of the Cretaceous period is not fully understood. Such massive amounts
/ K; r/ J( V6 W* f2 iof chalky sediments have never since been deposited over a comparable period of time.
0 w/ P; y7 g6 N, \The high biological productivity of the Cretaceous oceans also led to ideal conditions
9 B4 A/ Z1 P2 ~2 ?" A4 V! j2 m(20) for oil accumulation. Oil is formed when organic material trapped in sediments is slowly
* Y7 c% s# e6 }buried and subjected to increased temperatures and pressures, transforming it into# r; m" y( P5 _& D. N
petroleum. Sediments rich in organic material accumulated along the margins of the
& t$ t2 C) h9 g: M! C; KTethys Seaway, the tropical east-west ocean that formed when Earth's single landmass
# ?; |) [3 t6 ]# }0 u. o. [; T, \(known as Pangaea) split apart during the Mesozoic era. Many of today's important oil9 Q/ r4 k v: @. `0 o+ [
(25) fields are found in those sediments--in Russia, the Middle East, the Gulf of Mexico, and
+ W& I, X- I0 y3 A6 U" kin the states of Texas and Louisiana in the United States.) J# j% u4 ]4 O) s" E+ ^' c) S
/ c4 B, M" D( j5 }
) F% @" J1 |# A+ o3 Z
7 s/ T/ o ?. Q" G31. What does the passage mainly discuss?8 V* L; t0 J$ R( \: D* F
(A) How sediments were built up in oceans during the Cretaceous period4 `/ Q7 X: F2 k& I
(B) How petroleum was formed in the Mesozoic era
p! q+ D3 o' G1 }' j0 c. f(C) The impact of changes in oceanic animal and plant life in the Mesozoic era
% P8 Q6 ^5 ?' Q(D) The differences between plankton found in the present era and Cretaceous plankton |