Analysis of information sources in references of the Wikipedia article "Indonesia" in Indonesian language version.
The rise, of ca 60m, took place over most of the Earth as the volume of the oceans increased during deglaciation and is dated at 11,650–7000 cal. BP. The EHSLR was largely driven by meltwater release from decaying ice masses and the break up of coastal ice streams. [...] The impact of the EHSLR on climate is reviewed and it is maintained that the event was a factor in the 8200 BP cooling event, as well as in changes in ocean current patterns and their resultant effects. The EHSLR may also have enhanced volcanic activity, but no clear evidence of a causal link with submarine sliding on continental slopes and shelves can yet be demonstrated. The rise probably influenced rates and patterns of human migrations and cultural changes.
The rise, of ca 60m, took place over most of the Earth as the volume of the oceans increased during deglaciation and is dated at 11,650–7000 cal. BP. The EHSLR was largely driven by meltwater release from decaying ice masses and the break up of coastal ice streams. [...] The impact of the EHSLR on climate is reviewed and it is maintained that the event was a factor in the 8200 BP cooling event, as well as in changes in ocean current patterns and their resultant effects. The EHSLR may also have enhanced volcanic activity, but no clear evidence of a causal link with submarine sliding on continental slopes and shelves can yet be demonstrated. The rise probably influenced rates and patterns of human migrations and cultural changes.
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(bantuan) tanggal 1 Mei 2018. Diakses tanggal 5 Oktober 2006. "Salinan arsip". Archived from the original on 2018-05-01. Diakses tanggal 2008-07-29.|url=
(bantuan) tanggal 1 Mei 2018. Diakses tanggal 5 Oktober 2006. "Salinan arsip". Archived from the original on 2018-05-01. Diakses tanggal 2008-07-29.