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Lincoln University

Primary plant succession at Franz Josef Glacier: Aspects of predictability and ecophysiology: A dissertation submitted in partial fulfilment of the requirement for the Degree of Bachelor of Horticultural Science (Honours) at Lincoln University

Abstract

dc:description

8 distinct sites were selected from a previous study of plant succession and pedogenesis at Franz Josef Glacier by Stevens (1963; 1968). Plant species diversity and abundance were recorded on the 3 youngest sites, aged 45 to 85 years in the present study. Floristic composition was compared to composition recorded on the same sites 30 years previously. Sites in the present study were also compared to sites in the previous study, that were of equivalent age. Floristic composition did not appear to occur in a predictable manner, due to a dynamically changing understorey. Soil N levels were determined on all 8 successional sites. Total soil N increased over time, with initially rapid rates of accumulation declining with succession. The pattern of accumulation observed in the present study, was the same as that noted by Stevens (1963), confirming that N is increasing during early succession and pedogenesis. Total leaf N was determined for 3 species, Griselinia littoralis, Pseudopanax colensoi and Coprosma lucida, on each site. Leaf N (mg/g) was highly variable exhibiting no clear trends. Leaf N per unit leaf area (mg/cm² ) declined with increasing surface age and increasing specific leaf area (SLA). Leaf N did not correlate with soil N. This may be due to soil N availability levels declining, with increasing C/N ratios, associated with succession, or the inability of these species to utilise higher N. Chlorophyll levels and SLA were determined for the same 3 species, on the youngest and oldest sites of the successional sequence. An increase in SLA and total chlorophyll per weight (mg/g), and a decline in the chlorophyll a:b ratio suggest evidence of shade acclimation in these species.

Degree

thesis:*
Grantor dc:publisher
Lincoln University
Year dc:date
1991

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • McCorkindale, S. J.

Subjects

dc:subject × 11

Rights

dc:rights
Statement dc:rights
  • Digital thesis can be viewed by current staff and students of Lincoln University only. If you are the author of this item, please contact us if you wish to discuss making the full text publicly available.
Language dc:language
en

Identifiers

dc:identifier.*
Handle dc:identifier
https://hdl.handle.net/10182/15532
OAI identifier oai:identifier
oai:researcharchive.lincoln.ac.nz:10182/15532

Chain of custody

source
Harvested from
Lincoln University
Base URL
researcharchive.lincoln.ac.nz/dspace-oai/request
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
citation

McCorkindale, S. J.. Primary plant succession at Franz Josef Glacier: Aspects of predictability and ecophysiology: A dissertation submitted in partial fulfilment of the requirement for the Degree of Bachelor of Horticultural Science (Honours) at Lincoln University. Lincoln University, 1991. https://hdl.handle.net/10182/15532