Matches in climatepub4-kg for { <http://example.org/resource/d2d0ac71-d27d-46cb-b95b-39a6f796c501> ?p ?o ?g. }
Showing items 1 to 9 of
9
with 100 items per page.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 definition "The Neoarchean spans the period from 2,800 to 2,500 million years ago. During this era, oxygenic photosynthesis first evolved, releasing an abundance of oxygen, that first reacted with minerals and afterward was free to react with greenhouse gases of the atmosphere, leaving the Earth's surface free to radiate its energy to space. This is known as the oxygen catastrophe which was to happen later in the Paleoproterozoic from a poisonous buildup of oxygen in the atmosphere, released by these oxygen producing photoautotrophs, which evolved earlier in the Neoarchean." @default.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 id "1648655" @default.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 path_id 7160e90a-d7c4-4817-9b1c-e82211688bdb @default.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 path_id a9f88ca9-5d19-45fa-8fbb-3c6ff5f1f190 @default.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 path_label "ARCHAEAN" @default.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 path_label "Chronostratigraphic Units" @default.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 prefLabel "NEOARCHEAN" @default.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 reference "International Commission on Stratigraphy (http://www.stratigraphy.org/)" @default.
- d2d0ac71-d27d-46cb-b95b-39a6f796c501 tag "Chronostratigraphic Units" @default.