Overlapping markers can be separated by clicking on them.
Hovering the cursor over a marker will show the site's name.
Clicking on a marker will show information available about the collection site. (Compare with corresponding letter in table.)
| site | collection date | depth | substrate | salin | locality kind | comments | reference | |
|---|---|---|---|---|---|---|---|---|
| A | Lake Fenton, Tasmania, Australia | 1932 | freshwater | default type | alpine tableland of Central Plateau, 3400 ft of Tasmania. Geology include erratics, cirques, and glacial lakes. Moors covered with a thick peaty soil, which is wet throughout the year. Found in temporary pools formed by rain from Lake Fenton to Wo | Hickman VV (1933) 256, 267 | ||
| B | Mount Field National Park, Tasmania, Australia | 1932 | freshwater | default type | alpine tableland of Central Plateau, 3400 ft of Tasmania. Geology include erratics, cirques, and glacial lakes. Moors covered with a thick peaty soil, which is wet throughout the year. Found in temporary pools formed by rain from Lake Fenton to Wo | Hickman VV (1933) 256, 267 | ||
| C | Tasmania Island, Australia | 1932 | freshwater | default type | alpine tableland of Central Plateau, 3400 ft of Tasmania. Geology include erratics, cirques, and glacial lakes. Moors covered with a thick peaty soil, which is wet throughout the year. Found in temporary pools formed by rain from Lake Fenton to Wo | Hickman VV (1933) 256, 267 |