Skinner dkk 2004

@KT HIDUP DI JAMAN INTERGLASIAL
#For most of the past 2 million years [2 jt th terakhir], Erath’s climate was colder than at present. We live in an interglaciation within the late Cenozoic glacial ages that have dominated Earth’s recent climate [p.521]
#Our interglacial interval is now approximately 12,000 years old, close to the age where a return to glacial conditions might be expected [p.521]

@RENTANG WAKTU EARLY HOLOCENE & IKLIM PD MASA ITU
#Of particular interest are the EARLY HOLOCENE, from 11,000 to about 6000 ya when average temperatures were 0.5 to 10C warmer, & the warmest part of the last interglaciation, about 120,000 ya, when global temperatures were 1 to 20C higher [p.521]

@PELAPUKAN [10-11-14Sn lab mikropal hr pahlawan]
p.152
Air sangat berperan dlm proses pelapukan secara kimiawi krn dl air mengandung unsur-unsur CO2 & O2 yg larut didlmx.

Proses pelapukan secara kimiawi ini lebih cepat berjln di kawasan troppis yng mempunyai curah hujan yg tinggi dibandingkan dikawasan gurun misalx
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[7-11-15St vbm]






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