INDONESIAN THROUGHFLOW DYNAMICS ANALYSIS DURING THE LAST GLACIAL MAXIMUM USING PLANKTONIC FORAMINIFERA IN THE MAKASSAR STRAIT
Last Glacial Maximum (LGM) is a period when the Earth is in a cold phase and there is a massive formation of ice mass on land and in the sea at high latitudes. During the LGM, the climate conditions at high latitudes in the Northern Hemisphere were much colder compared to current conditions. T...
Saved in:
Main Author: | Dwi Demia Larasati, Oktavira |
---|---|
Format: | Theses |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/84573 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Similar Items
-
THE INTENSITY OF INDONESIAN THROUGHFLOW (ITF) DURING THE HEINRICH STADIAL 1 PERIOD IN THE MAKASSAR STRAIT USING PLANKTONIC FORAMINIFERA APPROACH
by: Sitalaksmi Siagian, Niken -
PLANKTONIC FORAMINIFERA ABUNDANCE AND ORIGIN POSSIBILITY ALONG THE INDONESIAN THROUGHFLOW
by: Romika Junita, Dynda -
SLOWDOWN OF INDONESIAN THROUGHFLOW INTENSITY IN THE MAKASSAR STRAIT OVER THE LAST DEGLACIATION
by: Hendrizan, Marfasran -
VARIABILITY ANALYSIS OF INDONESIAN THROUGHFLOW IN MAKASSAR STRAIT : Abstract
by: Galsan Mahie <br> NIM. 224 02 006, Andi -
ANALYSIS OF MARINE ECOLOGY DURING THE LAST WARMING PERIOD OF BÃLLING-ALLERÃD BASED ON THE ABUNDANCE AND DIVERSITY OF PLANKTONIC FORAMINIFERA IN THE MAKASSAR STRAIT
by: Rachmawati Purnomo, Maharani