Southeast Indian Ocean (244–675 CE): Ecological Consolidation…
244 CE to 675 CE
Southeast Indian Ocean (244–675 CE): Ecological Consolidation
Geographic & Environmental Context
The subregion of Southeast Indian Ocean includes Kerguelen east of 70°E and Heard Island and McDonald Islands. Eastern Kerguelen’s basaltic highlands and fjord systems defined the landscape, while Heard Island’s Big Ben retained summit ice and coastal glaciers. The McDonald Islands persisted as small, volcanically active islets buffeted by constant seas.
Anchors
- Kelp-rich coasts
- Seal rookeries
- Peatland basins
- Heard coastal margins
Climate & Environmental Conditions
Glacier retreat and advance remained modest, while ecological communities expanded and stabilized across coastal environments.
Ecological Setting
Peatlands thickened, vegetation mosaics broadened, and seal and seabird colonies became enduring landscape features.