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Tabl e 6. 3 Landmark articles in the top three specialties of mass extinctions (Citations 50)
Factor loadings
Name
Year
Source
Volume
Page
KT impact
0.964
Smit J
1980
Nature
285
198
0.918
Hildebrand AR
1991
Geology
19
867
0.917
Keller G
1993
Geology
21
776
0.887
Glen W
1994
Mass Extinction Deba
0.879
Sharpton VL
1992
Nature
359
819
0.877
Alvarez LW
1980
Science
208
1,095
Periodicity
0.898
Patterson C
1987
Nature
330
248
0.873
Raup DM
1986
Science
231
833
0.859
Raup DM
1984
P Natl Acad Sci-Biol
81
801
0.720
Jablonski D
1986
Dynamics Extinction
183
0.679
Benton MJ
1985
Nature
316
811
0.629
Davis M
1984
Nature
308
715
0.608
Jablonski D
1986
Science
231
129
Permian extinction
0.812
Magaritz M
1989
Geology
17
337
0.444
Renne PR
1995
Science
269
1,413
0.436
Stanley SM
1994
Science
266
1,340
0.426
Erwin DH
1994
Nature
367
231
0.425
Wignall PB
1996
Science
272
1,155
6.3.2.2
The Periodicity of Mass Extinctions
The second largest area in the visualization landscape highlights the theme of
the periodicity of mass extinctions. The periodicity frame in Fig. 6.9 shows two
predominant landmarks, both from David Raup and John Sepkoski. The one on the
left is their 1984 article published in the Proceedings of the National Academy of
Sciences of the United States of America - Biological Sciences, entitled Periodicity
of extinctions in the geologic past . They showed a graph of incidences of extinction
of marine families through time, in which peaks coincided with the time of most
major extinction events, and suggested that mass extinctions occurred every 26
million years. The one on the right is their 1982 article in Science , entitled Mass
extinctions in the marine fossil record .
The catastrophism was one of the major beneficiaries of the periodicity paradigm
because only astronomical forces are known to be capable of producing such a
precise periodic cycle. There were also hypotheses that attempted to incorporate
various terrestrial extinction-making events such as volcanism, global climatic
change, and glaciations. There was even a theory that each time an impact triggered
the volcanic plume, but supporting evidence was rather limited. A few landmark
articles in the periodicity frame addressed the causes of the periodicity of mass
extinctions using the impact paradigm with a hypothesis that asteroids or comets
strike the earth catastrophically every 26 million years.
 
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