The distribution and extent of Sphagnum moss on Macquarie Island

This indicator is no longer maintained, and is considered OBSOLETE. INDICATOR DEFINITION The locations where Sphagnum moss occurs on Macquarie Island including new occurrences and changes in the extent of Sphagnum moss at specific sites. TYPE OF INDICATOR There are three types of indicators used in...

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Bibliographic Details
Other Authors: WHINAM, JENNIFER (hasPrincipalInvestigator), WHINAM, JENNIFER (processor), Australian Antarctic Data Centre (publisher)
Format: Dataset
Language:unknown
Published: Australian Antarctic Data Centre
Subjects:
Online Access:https://researchdata.ands.org.au/distribution-extent-sphagnum-macquarie-island/701784
https://doi.org/10.26179/5d39034882771
https://data.aad.gov.au/metadata/records/SOE_sphagnum
http://nla.gov.au/nla.party-617536
Description
Summary:This indicator is no longer maintained, and is considered OBSOLETE. INDICATOR DEFINITION The locations where Sphagnum moss occurs on Macquarie Island including new occurrences and changes in the extent of Sphagnum moss at specific sites. TYPE OF INDICATOR There are three types of indicators used in this report: 1.Describes the CONDITION of important elements of a system; 2.Show the extent of the major PRESSURES exerted on a system; 3.Determine RESPONSES to either condition or changes in the condition of a system. This indicator is one of: CONDITION RATIONALE FOR INDICATOR SELECTION Non-vascular plant species are likely to be among the first plant taxa to respond to changes in climate. Sphagnum moss is present throughout montane, sub-alpine and alpine areas in eastern Australia, but is currently in decline and may become locally extinct with forecast changes in climate (Whinam and Chilcott, submitted). While small Sphagnum moss beds have been recorded on Macquarie Island for some time (Seppelt, 1984), there has been a marked expansion in both the number and size of these Sphagnum moss beds, which corresponds to an increase in temperatures recorded on the island (Whinam, unpubl. Data). Continuous Meteorology Bureau data are available for Macquarie Island since 1948. This indicator monitors both the occurrence of Sphagnum moss beds, including new records, as well as changes in extent of established Sphagnum moss beds on Macquarie Island over time. The increase in, and expansion of, these moss beds is a measure of how the non-vascular vegetation is responding to changed climatic conditions. DESIGN AND STRATEGY FOR INDICATOR MONITORING PROGRAM Spatial scale: Macquarie Island; Island wide distribution and 23 specified sites for extent, shown below with their TASPAWS grid reference. Site No - Name - Grid Ref 12 - Scoble Lake - 092 597 26 - Douglas Point - 065 568 31 - Square Lake - 084 537 32 - Above Square Lake - 091 535 33 - Above Square Lake - 091 537 34 - Tarn above Tulloch Lake - 085 532 36 - Handspike - 087 616 36 - Handspike - 087 616 38 - Green Gorge - 086 466 52 - Green Gorge - 086 466 53 - Green Gorge - 085 468 62 - Green Gorge - 085 465 63 - Green Gorge - 086 466 64 - Brothers Track - 088 496 65 - West of Brothers Lake - 091 509 66 - Above Tulloch Lake - 086 529 67 - Mawson Point - 065 547 68 - Mawson Point - 065 547 69 - Douglas Point - 065 568 70 - Eagle Point - 070 589 77 - Green Gorge - 086 467 81 - Handspike - 086 617 Frequency: Ground surveys of the island will be conducted every five years to record changes in distribution (subject to funding and shipping schedules), and would take approximately 10 days. Time to survey changes in areal extent of the established monitoring sites is approximately 7-10 days, weather permitting, for two people. This will take place every 2-3 years, subject to funding and shipping schedules. Measurement technique: The measurements are undertaken with GPS and tape measures. Every 5-10 years more accurate surveying by theodolite would be justified. Time series analysis will be used to explore the data. RESEARCH ISSUES The importance of continuous meteorology data to all projects involving climate change needs to be stressed. The availability of a topographic map with vegetation communities has greatly assisted this (and other) projects. The availability of a surveyor every 5-10 years to undertake more precise measurements than is possible with site maps and tape measures would add to the accuracy of data collected. LINKS TO OTHER INDICATORS Monthly averages of daily maximum and minimum temperatures Monthly extremes of daily maximum and minimum temperatures