Matches in climatepub4-kg for { <http://example.org/resource/3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2> ?p ?o ?g. }
Showing items 1 to 15 of
15
with 100 items per page.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 definition "Sediment - can be analyzed in many ways. Sediment laminations, or layers, can indicate sedimentation rate through time. Charcoal trapped in sediments can indicate past fire events. Remains of microorganisms such as diatoms, foraminifera, microbiota, and pollen within sediment can indicate changes in past climate, since each species has a limited range of habitable conditions. When these organisms and pollen sink to the bottom of a lake or ocean, they can become buried within the sediment. Thus, climate change can be inferred by species composition within the sediment." @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 id "1661898" @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_id 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_id 23703b6b-ee15-4512-b5b2-f441547e2edf @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_id 6f6423e8-ab4e-4572-8982-d9c40f64e28b @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_id c9a5b3eb-7556-41a8-a2b8-c015db80e5b2 @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_id e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_label "CLIMATE INDICATORS" @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_label "EARTH SCIENCE" @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_label "PALEOCLIMATE INDICATORS" @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_label "PALEOCLIMATE RECONSTRUCTIONS" @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 path_label "Science Keywords" @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 prefLabel "SEDIMENTS" @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 reference "Microbial Life - Montana State University - http://serc.carleton.edu/microbelife/topics/proxies/paleoclimate.html" @default.
- 3b4ea1db-bb93-4eb8-ac08-4880a3a5e6d2 tag "Science Keywords" @default.