Hays, Imbrie & Shackleton (1976) Science paper
GPTKB entity
Statements (21)
| Predicate | Object |
|---|---|
| gptkbp:instanceOf |
gptkb:academic_journal
|
| gptkbp:author |
gptkb:Nicholas_J._Shackleton
gptkb:James_D._Hays gptkb:John_Imbrie |
| gptkbp:citation |
over 5000
|
| gptkbp:doi |
10.1126/science.194.4270.1121
|
| https://www.w3.org/2000/01/rdf-schema#label |
Hays, Imbrie & Shackleton (1976) Science paper
|
| gptkbp:impact |
provided strong evidence for the Milankovitch theory of ice ages
|
| gptkbp:language |
English
|
| gptkbp:method |
analysis of deep-sea sediment cores
|
| gptkbp:pages |
1121-1132
|
| gptkbp:plotSummary |
Earth's climate changes are paced by variations in its orbit
|
| gptkbp:publicationYear |
1976
|
| gptkbp:publishedIn |
gptkb:science
|
| gptkbp:subject |
gptkb:Milankovitch_cycles
paleoclimatology ice ages |
| gptkbp:title |
gptkb:Variations_in_the_Earth's_Orbit:_Pacemaker_of_the_Ice_Ages
|
| gptkbp:volume |
194
|
| gptkbp:bfsParent |
gptkb:James_D._Hays
|
| gptkbp:bfsLayer |
6
|