Taphonomy

Taphonomy is the study of how organisms decay and become fossilized . The term taphonomy (from the Greek taphos , τάφος meaning "burial", and nomos , νόμος meaning "law") was introduced to paleontology in 1949 [1] by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms from the biosphere to the lithosphere . [2] [3]

Page Revisions

Year Metadata Sections Top Words First Paragraph
2018

99819 characters

21 sections

31 paragraphs

8 images

187 internal links

48 external links

1. Description

2. Research areas

3. Taphonomic biases in the fossil record

4. Preservation of biopolymers

5. Disintegration

6. Significance

7. See also

8. References

9. Further reading

10. External links

fossil 0.332

taphonomic 0.284

taphonomy 0.263

fossils 0.229

organisms 0.209

burial 0.201

preservation 0.171

organism 0.161

record 0.156

tissue 0.149

bias 0.121

cuticle 0.114

scavengers 0.114

deposit 0.110

fossilization 0.103

Taphonomy is the study of how organisms decay and become fossilized . The term taphonomy (from the Greek taphos , τάφος meaning "burial", and nomos , νόμος meaning "law") was introduced to paleontology in 1949 [1] by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms from the biosphere to the lithosphere . [2] [3]

2017

96787 characters

21 sections

31 paragraphs

8 images

182 internal links

43 external links

1. Description

2. Research areas

3. Taphonomic biases in the fossil record

4. Preservation of biopolymers

5. Disintegration

6. Significance

7. See also

8. References

9. Further reading

10. External links

fossil 0.332

taphonomic 0.284

taphonomy 0.263

fossils 0.229

organisms 0.209

burial 0.201

preservation 0.171

organism 0.161

record 0.156

tissue 0.149

bias 0.121

cuticle 0.114

scavengers 0.114

deposit 0.110

fossilization 0.103

Taphonomy is the study of how organisms decay and become fossilized . The term taphonomy (from the Greek taphos , τάφος meaning "burial", and nomos , νόμος meaning "law") was introduced to paleontology in 1949 [1] by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms from the biosphere to the lithosphere . [2] [3]

2016

163284 characters

17 sections

26 paragraphs

10 images

237 internal links

35 external links

1. Description

2. Research areas

3. Taphonomic biases in the fossil record

4. Preservation of biopolymers

5. Disintegration

6. See also

7. References

8. Further reading

9. External links

fossil 0.400

organisms 0.279

fossils 0.275

preservation 0.206

taphonomic 0.205

tissue 0.179

record 0.177

taphonomy 0.169

bias 0.167

cuticle 0.137

deposit 0.132

overrepresented 0.123

biota 0.110

biased 0.094

pollen 0.093

Taphonomy is the study of decaying organisms over time and how they may become fossilized . The term taphonomy (from the Greek taphos , τάφος meaning "burial", and nomos , νόμος meaning "law") was introduced to paleontology in 1940 by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2015

82637 characters

17 sections

26 paragraphs

6 images

175 internal links

34 external links

1. Description

2. Research areas

3. Taphonomic biases in the fossil record

4. Preservation of biopolymers

5. Disintegration

6. See also

7. References

8. Further reading

9. External links

fossil 0.400

organisms 0.279

fossils 0.275

preservation 0.206

taphonomic 0.205

tissue 0.179

record 0.177

taphonomy 0.169

bias 0.167

cuticle 0.137

deposit 0.132

overrepresented 0.123

biota 0.110

biased 0.094

pollen 0.093

Taphonomy is the study of decaying organisms over time and how they may become fossilized . The term taphonomy (from the Greek taphos , τάφος meaning "burial", and nomos , νόμος meaning "law") was introduced to paleontology in 1940 by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2014

76284 characters

17 sections

26 paragraphs

6 images

181 internal links

26 external links

1. Description

2. Research areas

3. Taphonomic biases in the fossil record

4. Preservation of biopolymers

5. Disintegration

6. See also

7. References

8. Further reading

9. External links

fossil 0.400

organisms 0.279

fossils 0.275

preservation 0.206

taphonomic 0.205

tissue 0.179

record 0.177

taphonomy 0.169

bias 0.167

cuticle 0.137

deposit 0.132

overrepresented 0.123

biota 0.110

biased 0.094

pollen 0.093

Taphonomy is the study of decaying organisms over time and how they may become fossilized . The term taphonomy (from the Greek taphos , τάφος meaning burial, and nomos , νόμος meaning law) was introduced to paleontology in 1940 by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2013

61613 characters

16 sections

24 paragraphs

6 images

151 internal links

16 external links

1. Description

2. Research areas

3. Taphonomic biases in the fossil record

4. Preservation of biopolymers

5. Disintegration

6. See also

7. References

8. Further reading

9. External links

fossil 0.407

organisms 0.284

fossils 0.263

preservation 0.209

taphonomic 0.209

tissue 0.182

record 0.180

bias 0.170

taphonomy 0.151

cuticle 0.139

deposit 0.134

overrepresented 0.126

biota 0.112

biased 0.096

pollen 0.094

Taphonomy is the study of decaying organisms over time and how they become fossilized (if they do). The term taphonomy (from the Greek taphos , τάφος meaning burial, and nomos , νόμος meaning law) was introduced to paleontology in 1940 by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2012

60129 characters

15 sections

24 paragraphs

6 images

149 internal links

16 external links

1. Description

2. Research areas

3. Taphonomic biases in the fossil record

4. Preservation of biopolymers

5. Disintegration

6. See also

7. References

8. Further reading

9. External links

fossil 0.369

preservation 0.264

organisms 0.259

bias 0.226

fossils 0.224

taphonomic 0.223

record 0.179

tissue 0.167

taphonomy 0.161

cuticle 0.149

deposit 0.143

biota 0.120

biased 0.103

soft 0.098

remains 0.094

Taphonomy is the study of decaying organisms over time and how they become fossilized (if they do). The term taphonomy (from the Greek taphos - τάφος meaning burial, and nomos - νόμος meaning law) was introduced to paleontology in 1940 by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2011

47286 characters

14 sections

24 paragraphs

5 images

80 internal links

16 external links

1. Research areas

2. Taphonomic biases in the fossil record

3. Preservation of biopolymers

4. Disintegration

5. See also

6. References

7. Further reading

8. External links

fossil 0.373

preservation 0.267

organisms 0.262

bias 0.229

taphonomic 0.225

fossils 0.189

record 0.181

tissue 0.168

taphonomy 0.163

cuticle 0.150

deposit 0.145

biota 0.121

biased 0.104

soft 0.099

remains 0.095

Taphonomy is the study of decaying organisms over time and how they become fossilized (if they do). The term taphonomy (from the Greek taphos - τάφος meaning burial, and nomos - νόμος meaning law) was introduced to paleontology in 1940 by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2010

45870 characters

14 sections

23 paragraphs

4 images

76 internal links

16 external links

1. Research areas

2. Taphonomic biases in the fossil record

3. Preservation of biopolymers

4. Notes

5. See also

6. References

7. Further reading

8. External links

fossil 0.377

preservation 0.269

organisms 0.265

bias 0.231

taphonomic 0.227

record 0.183

fossils 0.172

tissue 0.170

taphonomy 0.164

cuticle 0.152

deposit 0.146

biota 0.122

biased 0.105

soft 0.100

remains 0.096

Taphonomy [note 1] is the study of decaying organisms over time and how they become fossilized (if they do). The term taphonomy, (from the Greek taphos - τάφος meaning burial, and nomos - νόμος meaning law), was introduced to paleontology in 1940 by Russian scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2009

29316 characters

5 sections

12 paragraphs

4 images

45 internal links

16 external links

1. Preservation of biopolymers

2. Notes

3. References

4. Further reading

5. External links

taphonomic 0.329

preservation 0.287

cuticle 0.263

tissue 0.246

organisms 0.204

fossil 0.192

taphonomy 0.163

sclerobionts 0.131

cutan 0.131

soft 0.124

remains 0.116

paleontologists 0.106

renders 0.102

prone 0.093

tissues 0.091

Taphonomy [note 1] is the study of decaying organisms over time and how they become fossilized (if they do). The term taphonomy, (from the Greek taphos - τάφος meaning burial, and nomos - νόμος meaning law), was introduced to paleontology in 1940 by Russian scientist, Ivan Efremov , to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2008

26208 characters

4 sections

12 paragraphs

2 images

38 internal links

16 external links

1. Preservation of biopolymers

2. References

3. Further reading

4. External links

taphonomic 0.328

preservation 0.287

cuticle 0.262

tissue 0.245

organisms 0.204

fossil 0.192

taphonomy 0.162

sclerobionts 0.131

cutan 0.131

soft 0.124

remains 0.116

paleontologists 0.106

renders 0.101

prone 0.093

tissues 0.091

Taphonomy is the study of decaying organisms over time and how they become fossilized (if they do). The term taphonomy, (from the Greek taphos - τάφος meaning burial, and nomos - νόμος meaning law), was introduced to paleontology in 1940 by Russian scientist, Ivan Efremov , to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages. [1] [2]

2007

10379 characters

2 sections

6 paragraphs

3 images

27 internal links

5 external links

1. References

2. External links

taphonomic 0.383

taphonomy 0.296

fossil 0.280

remains 0.218

paleontologists 0.154

study 0.149

doctoral 0.148

archaeological 0.143

excavated 0.127

organism 0.120

decomposition 0.120

organisms 0.111

animal 0.105

processes 0.099

record 0.099

Taphonomy is the study of a decaying organism over time. The term taphonomy, (from the Greek taphos meaning burial, and nomos meaning law), was introduced to paleontology in 1940 by Russian scientist, Ivan Efremov , to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages, ( e.g. see Shipman 1981 p.5-6, Greenwood 1991, Lyman 1994).

2006

6740 characters

2 sections

6 paragraphs

0 images

20 internal links

2 external links

1. References

2. External links

taphonomic 0.400

fossil 0.293

taphonomy 0.247

remains 0.228

paleontologists 0.161

doctoral 0.155

archaeological 0.150

study 0.139

excavated 0.132

organism 0.126

decomposition 0.126

organisms 0.116

animal 0.109

processes 0.103

record 0.103

Taphonomy is the study of a decaying organism over time. The term taphonomy, (from the Greek taphos meaning burial, and nomos meaning law), was introduced to paleontology in 1940 by Russian scientist, Ivan Efremov , to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages, ( e.g. see Shipman 1981 p.5-6, Greenwood 1991, Lyman 1994).

2005

4761 characters

2 sections

5 paragraphs

0 images

13 internal links

2 external links

1. References

2. External links

taphonomy 0.342

fossil 0.324

remains 0.280

taphonomic 0.276

organisms 0.215

decomposition 0.174

processes 0.143

biostratinomy 0.138

efremov 0.138

ivan 0.138

taphos 0.138

diagenesis 0.125

fossilization 0.125

assemblage 0.125

nomos 0.125

Taphonomy is the study of the fate of the remains of organisms after they die. The term taphonomy, (from the Greek taphos meaning burial, and nomos meaning law), was introduced to palaeontology in 1940 by Russian scientist, Ivan Efremov , to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages, ( e.g. see Shipman 1981 p.5-6, Greenwood 1991, Lyman 1994).

2004

3922 characters

2 sections

4 paragraphs

0 images

11 internal links

2 external links

1. References

2. External links

taphonomy 0.405

fossil 0.383

organisms 0.254

decomposition 0.206

remains 0.165

biostratinomy 0.164

efremov 0.164

taphos 0.164

diagenesis 0.148

fossilization 0.148

assemblage 0.148

nomos 0.148

paleontologists 0.132

biases 0.127

assemblages 0.122

Taphonomy is the study of the fate of the remains of organisms after they die. The term taphonomy, (from the Greek taphos meaning burial, and nomos meaning law), was introduced to palaeontology in 1940 by a Russian scientist, Efremov, to describe the study of the transition of remains, parts, or products of organisms , from the biosphere , to the lithosphere , i.e. the creation of fossil assemblages, ( e.g. see Shipman 1981 p.5-6, Greenwood 1991).

2003

989 characters

0 sections

1 paragraphs

0 images

3 internal links

0 external links

decomposition 0.418

taphonomy 0.411

die 0.405

fate 0.367

fossils 0.334

phenomena 0.310

organisms 0.258

bodies 0.169

studies 0.151

formation 0.137

study 0.115

Taphonomy is the study of the fate of the bodies of organisms after they die. It studies such phenomena as decomposition and the formation of fossils .