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[历年真题] 托福阅读历年真题精选30

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发表于 2012-8-14 22:34:35 | 显示全部楼层 |阅读模式
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
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 楼主| 发表于 2012-8-14 22:34:36 | 显示全部楼层

托福阅读历年真题精选30

32. The passage indicates that the Creiaceous period occurred</p>(A) in the early part of the Mesozoic era
3 H+ v. w4 R) r2 b(B) in the middle part of the Mesozoic era
8 f7 \2 E. `  e7 H! i(C) in the later part of the Mesozoic era# G4 _" j' z2 y, \/ N2 Y
(D) after the Mesozoic era$ a5 S* U9 J$ _' }7 Q5 d

, @# X7 H( g# Q) y6 H* e33. The passage mentions all of the following aspects of plankton EXCEPT2 D* k, V# C+ Q. a1 J4 |) f
(A) the length of their lives
* O2 k( k5 }$ O3 I; f$ g" I(B) the level of the ocean at which they are found- s9 `/ I3 Q5 w( X3 k' ], e9 I
(C) their movement4 P' C. s5 ?8 y! h
(D) their size- `0 b+ n2 }: ]
1 Q, N: x0 X" U4 z) c4 |
34. The word "accumulated" in line 8 is closest in meaning to
( Y% ], i$ Y9 }/ L3 [(A) depended! o8 K2 Z" r9 m0 P/ K
(B) matured
7 Y- U  O7 O) r7 V7 `(C) dissolved
, J5 l. C) V4 ]" b9 F(D) collected
% ?* l, P) u1 \& d % t4 N2 `5 E, N+ Y& g
35. According to the passage, the most dramatic change to the oceans caused by plankton during5 N  }" n/ r9 z" k. `* J% k, L
the Cretaceous period concerned
9 @$ r. Y. o0 p" m4 t' G(A) the depth of the water$ m( {/ M5 g1 c) _# f- v4 B
(B) the makeup of the sediment on the ocean floor& [) j, Q+ O# d- m' x2 o4 n# F: q+ R
(C) the decrease in petroleum-producing sediment2 U8 n6 ]1 j9 A! K2 ]
(D) a decline in the quantity of calcareous ooze on the seafloor( f% `8 X4 R: Z- I; F  v
+ ?- j4 B( A4 g4 l
36. The "white chalk cliffs of Dover" are mentioned in line 14 of the passage to" ]0 Z: P! a7 ^$ Z  b8 d& \
(A) show where the plankton sediment first began to build up! l% _  g- w, f2 q# D: {
(B) provide an example of a plankton buildup that scientists cannot explain* \/ w  H1 Z) P5 T0 n( Z/ G
(C) provide an example of the buildup of plankton sediment
4 |! \7 a/ @& }(D) indicate the largest single plankton buildup on Earth; v0 u5 H  {5 f

% [) n% X) x2 L( H$ b37. The word "prolific" in line 16 is closest in meaning to
) |6 l) r& t  K+ Q( a4 T3 {. `(A) fruitful
$ s& d- d7 C  ~8 x(B) distinct6 L5 ~) r/ ^2 |, @0 P$ G. N  }
(C) determined& r$ `( D; c/ |. f. q/ W: T
(D) energetic
: ~4 }" E8 q7 g+ |. _' ?( o
8 I+ g8 {, N% o5 ]38. The word "ideal" in line 19 is closest in meaning to1 ~3 x' W9 D+ V* n6 M
(A) common. v3 a% x4 n! A) g! B: H2 Q
(B) clear( w' U! g) q. u; J4 l, J4 A# P/ M
(C) perfect
. R* \, e1 b: r' H- g6 r6 H(D) immediate
& D$ x1 E' P0 k: T" e( B, g7 z
$ d. z: z$ q! d! N7 B2 H39. The word "it" in line 21 refers to
6 Q4 Q, h) v" F! Y- R0 E7 O(A) biological productivity
* m' o" h) O' L(B) oil
, q$ ]- s5 c4 G+ K% J+ M6 J(C) organic material
9 D( `- n  |: c/ C5 i7 v(D) petroleum
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