Paleoclimatology
Paleoclimatology (in British spelling , palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within things such as rocks , sediments , ice sheets , tree rings , corals , shells , and microfossils . It then uses the records to determine the past states of the Earth 's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, specifically the impact of climate on mass extinctions and biotic recovery. [1]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
210626 characters 26 sections 32 paragraphs 21 images 446 internal links 80 external links |
2. Reconstructing ancient climates 3. Notable climate events in Earth history |
oxygen 0.250 ice 0.199 phanerozoic 0.156 geomorphology 0.143 atmosphere 0.130 eon 0.117 record 0.115 asymmetry 0.095 coring 0.095 nebula 0.095 rearrangement 0.095 subduction 0.095 climates 0.095 evolution 0.095 ring 0.095 |
Paleoclimatology (in British spelling , palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within things such as rocks , sediments , ice sheets , tree rings , corals , shells , and microfossils . It then uses the records to determine the past states of the Earth 's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, specifically the impact of climate on mass extinctions and biotic recovery. [1] |
| 2017 |
209060 characters 26 sections 31 paragraphs 21 images 447 internal links 70 external links |
2. Reconstructing ancient climates 3. Notable climate events in Earth history |
oxygen 0.256 ice 0.203 phanerozoic 0.159 geomorphology 0.146 atmosphere 0.139 eon 0.120 record 0.117 asymmetry 0.097 coring 0.097 nebula 0.097 rearrangement 0.097 subduction 0.097 climates 0.097 evolution 0.097 ring 0.097 |
Paleoclimatology (in British spelling , palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within things such as rocks , sediments , ice sheets , tree rings , corals , shells , and microfossils . It then uses the records to determine the past states of the Earth 's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, specifically the impact of climate on mass extinctions and biotic recovery. [1] |
| 2016 |
157367 characters 25 sections 30 paragraphs 16 images 403 internal links 60 external links |
2. Reconstructing ancient climates 3. Notable climate events in Earth history |
oxygen 0.266 ice 0.211 phanerozoic 0.166 atmosphere 0.145 eon 0.124 record 0.112 asymmetry 0.101 coring 0.101 nebula 0.101 rearrangement 0.101 subduction 0.101 evolution 0.100 ring 0.100 weathering 0.097 ago 0.097 |
Paleoclimatology (in British spelling , palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within things such as rocks , sediments , ice sheets , tree rings , corals , shells and microfossils . It then uses the records to determine the past states of the Earth 's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, specifically the impact of climate on mass extinctions and biotic recovery. [1] |
| 2015 |
149644 characters 24 sections 30 paragraphs 16 images 403 internal links 50 external links |
2. Reconstructing ancient climates 3. Notable climate events in Earth history |
oxygen 0.266 ice 0.211 phanerozoic 0.166 atmosphere 0.145 eon 0.124 record 0.112 asymmetry 0.101 coring 0.101 nebula 0.101 rearrangement 0.101 subduction 0.101 evolution 0.100 ring 0.100 weathering 0.097 ago 0.097 |
Paleoclimatology (in British spelling , palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within things such as rocks , sediments , ice sheets , tree rings , corals , shells and microfossils . It then uses the records to determine the past states of the Earth 's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, specifically the impact of climate on mass extinctions and biotic recovery. [1] |
| 2014 |
98999 characters 24 sections 30 paragraphs 11 images 193 internal links 38 external links |
2. Reconstructing ancient climates 3. Notable climate events in Earth history |
oxygen 0.268 ice 0.213 phanerozoic 0.167 atmosphere 0.146 eon 0.125 record 0.113 ago 0.109 asymmetry 0.102 coring 0.102 nebula 0.102 evolution 0.101 ring 0.101 weathering 0.098 core 0.097 masses 0.089 |
Paleoclimatology (in British spelling , palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within (e.g.) rocks , sediments , ice sheets , tree rings , corals , shells and microfossils ; it then uses these records to determine the past states of the Earth 's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, and specifically the impact of climate on mass extinctions and biotic recovery. [1] |
| 2013 |
109568 characters 24 sections 32 paragraphs 12 images 174 internal links 55 external links |
1. Reconstructing ancient climates 2. Notable climate events in Earth history |
galactic 0.325 ice 0.217 sun 0.170 phanerozoic 0.167 cosmic 0.163 solar 0.150 evolution 0.142 polar 0.132 spiral 0.122 motions 0.122 record 0.098 today 0.098 masses 0.095 sheets 0.088 plate 0.087 |
Template:Geology2 Paleoclimatology (in British spelling , palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within (e.g.) rocks , sediments , ice sheets , tree rings , corals , shells and microfossils ; it then uses these records to determine the past states of the Earth 's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, and specifically the impact of climate on mass extinctions and biotic recovery. [1] |
| 2012 |
99561 characters 21 sections 28 paragraphs 11 images 171 internal links 47 external links |
1. Reconstructing ancient climates 2. Notable climate events in Earth history |
galactic 0.353 sun 0.185 ice 0.184 cosmic 0.176 phanerozoic 0.145 solar 0.138 spiral 0.132 motions 0.132 polar 0.125 evolution 0.110 today 0.106 masses 0.103 core 0.101 plate 0.095 ray 0.088 |
Paleoclimatology (in British spelling , palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within (e.g.) rocks , sediments , ice sheets , tree rings , corals , shells and microfossils ; it then uses these records to determine the past states of the Earth 's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, and specifically the impact of climate on mass extinctions and biotic recovery. [1] |
| 2011 |
93716 characters 21 sections 28 paragraphs 9 images 162 internal links 42 external links |
1. Reconstructing ancient climates 2. Notable climate events in Earth history |
galactic 0.356 sun 0.186 ice 0.186 cosmic 0.178 phanerozoic 0.146 today 0.134 spiral 0.133 motions 0.133 polar 0.126 solar 0.114 evolution 0.111 masses 0.104 core 0.102 plate 0.096 ago 0.095 |
Paleoclimatology (also palaeoclimatology ) is the study of changes in climate taken on the scale of the entire history of Earth . It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within ( e.g. ) rocks , sediments , ice sheets , tree rings , corals , shells and microfossils ; it then uses these records to determine the past states of the Earth 's various climate regions and its atmospheric system. Paleoclimatology has wider implications for climate change today. Scientists often consider past changes in environment and biodiversity to reflect on the current situation, and specifically the impact of climate on mass extinctions and biotic recovery. [1] |
| 2010 |
96137 characters 21 sections 30 paragraphs 9 images 146 internal links 36 external links |
1. Reconstructing ancient climates |
galactic 0.360 sun 0.188 cosmic 0.180 phanerozoic 0.148 ice 0.137 today 0.135 spiral 0.135 motions 0.135 polar 0.128 solar 0.115 evolution 0.112 eon 0.111 timeline 0.111 masses 0.105 plate 0.097 |
Paleoclimatology (also Palaeoclimatology ) is the study of climate change taken on the scale of the entire history of Earth . It uses a variety of proxy records from ice sheets , tree rings , sediment , corals, shells and rocks to determine the past state of the climate system on Earth . |
| 2009 |
68251 characters 21 sections 29 paragraphs 8 images 116 internal links 21 external links |
1. Reconstructing ancient climates |
galactic 0.361 sun 0.189 cosmic 0.180 phanerozoic 0.148 ice 0.137 spiral 0.135 motions 0.135 polar 0.128 today 0.122 solar 0.115 evolution 0.112 eon 0.111 timeline 0.111 ago 0.106 masses 0.105 |
Paleoclimatology (also Palaeoclimatology ) is the study of climate change taken on the scale of the entire history of Earth . It uses records from ice sheets , tree rings , sediment , and rocks to determine the past state of the climate system on Earth . |
| 2008 |
57682 characters 19 sections 24 paragraphs 5 images 88 internal links 21 external links |
ma 0.453 galactic 0.362 eon 0.149 precambrian 0.149 ice 0.138 motions 0.136 poles 0.116 cambrian 0.112 timeline 0.112 masses 0.106 sun 0.103 o2 0.097 continental 0.092 polar 0.092 oxygen 0.092 |
Template:Reference-improve Paleoclimatology (also Palaeoclimatology ) is the study of climate change taken on the scale of the entire history of Earth . It uses records from ice sheets , tree rings , sediment , and rocks to determine the past state of the climate system on Earth . |
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| 2007 |
43406 characters 13 sections 24 paragraphs 3 images 92 internal links 16 external links |
ma 0.492 ice 0.178 eon 0.162 precambrian 0.162 rings 0.147 sedimentary 0.141 poles 0.126 cambrian 0.121 timeline 0.121 polar 0.120 masses 0.115 o2 0.106 continental 0.100 oxygen 0.100 asymmetry 0.098 |
Paleoclimatology (also Palaeoclimatology ) is the study of climate change taken on the scale of the entire history of Earth . It uses records from ice sheets , tree rings , sediment , and rocks to determine the past state of the climate system on Earth . |
|
| 2006 |
47332 characters 13 sections 24 paragraphs 5 images 117 internal links 13 external links |
ma 0.493 ice 0.187 eon 0.162 precambrian 0.162 sedimentary 0.141 poles 0.127 rings 0.123 cambrian 0.121 timeline 0.121 polar 0.120 masses 0.115 o2 0.106 continental 0.100 oxygen 0.100 asymmetry 0.099 |
Paleoclimatology is the study of climate change taken on the scale of the entire history of the Earth . |
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| 2005 |
42945 characters 12 sections 25 paragraphs 3 images 92 internal links 11 external links |
ma 0.474 eon 0.173 precambrian 0.173 ice 0.170 poles 0.135 cambrian 0.130 timeline 0.130 polar 0.128 masses 0.123 o2 0.113 continental 0.107 oxygen 0.107 asymmetry 0.105 rodinia 0.105 geologic 0.101 |
Paleoclimatology is the study of climate change taken on the scale of the entire history of the earth. |
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| 2004 |
17830 characters 11 sections 34 paragraphs 0 images 42 internal links 2 external links |
1. The beginning of Earth's climate |
tillites 0.300 cambrian 0.296 phanerozoic 0.197 precambrian 0.197 eons 0.180 banded 0.180 proterozoic 0.180 iron 0.172 earliest 0.161 eon 0.148 formations 0.148 o2 0.129 bacteria 0.129 life 0.126 beds 0.120 |
Paleoclimatology is the study of climate change taken on the scale of the entire history of the earth. |
| 2003 |
12881 characters 10 sections 29 paragraphs 0 images 35 internal links 1 external links |
tillites 0.316 cambrian 0.311 phanerozoic 0.207 precambrian 0.207 eons 0.189 banded 0.189 proterozoic 0.189 iron 0.181 earliest 0.170 eon 0.156 formations 0.156 o2 0.136 bacteria 0.136 life 0.132 beds 0.126 |
Paleoclimatology is the study of climate change taken on the scale of the entire history of the earth. |
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| 2002 |
8801 characters 0 sections 42 paragraphs 0 images 30 internal links 0 external links |
tillites 0.345 cambrian 0.340 banded 0.207 iron 0.198 earliest 0.186 eon 0.170 formations 0.170 precambrian 0.170 o2 0.148 bacteria 0.148 life 0.144 eons 0.138 beds 0.138 sex 0.138 oldest 0.133 |
Paleoclimatology is the study of climate change taken on the scale of the entire history of the earth. |