Maapallon kasvihuonetila ja jääkausitila (Finnish Wikipedia)

Analysis of information sources in references of the Wikipedia article "Maapallon kasvihuonetila ja jääkausitila" in Finnish language version.

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4web.archive.org

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2nature.com

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2doi.org

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2worldcat.org

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1ipa.org.au

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1rice.edu

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1springer.com

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1geoclimmodel.wordpress.com

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1nih.gov

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1pnas.org

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1euronet.nl

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doi.org

dx.doi.org

Yves Goddéris, Yannick Donnadieu, Sébastien Carretier, Markus Aretz, Guillaume Dera, Mélina Macouin: Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering. Nature Geoscience, 2017-05, nro 10, s. 382–386. doi:10.1038/ngeo2931 ISSN 1752-0908 Artikkelin verkkoversio. (englanniksi)
Georg Feulner: Formation of most of our coal brought Earth close to global glaciation. Proceedings of the National Academy of Sciences, 24.10.2017, nro 114, s. 11333–11337. PubMed:29073052 doi:10.1073/pnas.1712062114 ISSN 0027-8424 Artikkelin verkkoversio. (englanniksi) (Arkistoitu – Internet Archive)

euronet.nl

Evert Wesker: Climate Change; a summary of some present knowledge and theories (html) euronet.nl. Arkistoitu 7.12.2013. (englanniksi)

geoclimmodel.wordpress.com

The Late Paleozoic Ice Age and the Hercynian Orogeny GEOCLIM. 19.11.2017. Viitattu 4.12.2021. (englanniksi)

ipa.org.au

Plimer, Ian (2003) The Past is the Key to the Present: Greenhouse and Icehouse over time (Arkistoitu – Internet Archive)IPA Review 55,1. Institute of Public Affairs (Australia)

nature.com

Stephen F. Pekar (2008) Climate change: When did the icehouse cometh? Nature Reports Climate Change.
Yves Goddéris, Yannick Donnadieu, Sébastien Carretier, Markus Aretz, Guillaume Dera, Mélina Macouin: Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering. Nature Geoscience, 2017-05, nro 10, s. 382–386. doi:10.1038/ngeo2931 ISSN 1752-0908 Artikkelin verkkoversio. (englanniksi)

nih.gov

pubmed.ncbi.nlm.nih.gov

Georg Feulner: Formation of most of our coal brought Earth close to global glaciation. Proceedings of the National Academy of Sciences, 24.10.2017, nro 114, s. 11333–11337. PubMed:29073052 doi:10.1073/pnas.1712062114 ISSN 0027-8424 Artikkelin verkkoversio. (englanniksi) (Arkistoitu – Internet Archive)

pnas.org

Georg Feulner: Formation of most of our coal brought Earth close to global glaciation. Proceedings of the National Academy of Sciences, 24.10.2017, nro 114, s. 11333–11337. PubMed:29073052 doi:10.1073/pnas.1712062114 ISSN 0027-8424 Artikkelin verkkoversio. (englanniksi) (Arkistoitu – Internet Archive)

rice.edu

news.rice.edu

Volcano location could be greenhouse-icehouse key (Arkistoitu – Internet Archive) Rice University News & Media 8.2.2013

springer.com

Paul K. Link (2009) "Icehouse" (cold) climates. In: Encyclopedia of Paleoclimatology and Ancient Environments (V. Gornitz, ed.), 463–471. Springer, ISBN 978-1-4020-4551-6.

web.archive.org

Plimer, Ian (2003) The Past is the Key to the Present: Greenhouse and Icehouse over time (Arkistoitu – Internet Archive)IPA Review 55,1. Institute of Public Affairs (Australia)
Volcano location could be greenhouse-icehouse key (Arkistoitu – Internet Archive) Rice University News & Media 8.2.2013
Georg Feulner: Formation of most of our coal brought Earth close to global glaciation. Proceedings of the National Academy of Sciences, 24.10.2017, nro 114, s. 11333–11337. PubMed:29073052 doi:10.1073/pnas.1712062114 ISSN 0027-8424 Artikkelin verkkoversio. (englanniksi) (Arkistoitu – Internet Archive)
Evert Wesker: Climate Change; a summary of some present knowledge and theories (html) euronet.nl. Arkistoitu 7.12.2013. (englanniksi)

worldcat.org

Yves Goddéris, Yannick Donnadieu, Sébastien Carretier, Markus Aretz, Guillaume Dera, Mélina Macouin: Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering. Nature Geoscience, 2017-05, nro 10, s. 382–386. doi:10.1038/ngeo2931 ISSN 1752-0908 Artikkelin verkkoversio. (englanniksi)
Georg Feulner: Formation of most of our coal brought Earth close to global glaciation. Proceedings of the National Academy of Sciences, 24.10.2017, nro 114, s. 11333–11337. PubMed:29073052 doi:10.1073/pnas.1712062114 ISSN 0027-8424 Artikkelin verkkoversio. (englanniksi) (Arkistoitu – Internet Archive)