Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Ascarina lucida"'
Publikováno v:
Quaternary International. 184:129-138
Palynological studies from most of the drier eastern and southern parts of the South Island, New Zealand, suggest that the climate regime switched from prevailing northerly airflows to dominant south-westerly airflows during the mid to late Holocene.
Publikováno v:
Review of Palaeobotany and Palynology. 136:143-158
Vegetation and climate changes during the Last Glacial through to the late Holocene are identified by pollen analysis of a core from Lake Tangonge in far northern New Zealand. During the earliest part of the record (> 50 ka), regional vegetation was
Publikováno v:
Journal of Paleolimnology. 19:23-32
Late Holocene pollen and sediment records from the Lake Tauanui catchment, northern New Zealand, indicate that the lake formed about 5500 years ago following a series of volcanic events in the Tauanui Volcanic Centre. These volcanic events initiated
Autor:
Michael B. Elliot
Publikováno v:
Review of Palaeobotany and Palynology. 99:189-202
A vegetational history and palaeoclimatic changes are established for the last 25,000 yr by pollen analysis of two peat cores from Kaitaia Bog, far northern New Zealand. Twelve AMS radiocarbon dates provide a chronology covering the Last Glacial Maxi
Autor:
C. J. Burrows
Publikováno v:
New Zealand Journal of Botany. 34:509-515
Germination rates, percentage germination success, and phenomena related to germination delay were determined for seeds of Ascarina lucida, Coprosma grandifolia, Melicytus lanceolatus, and Solanum laciniatum, taken from freshly collected fruit. The e
Publikováno v:
Radiocarbon. 37:899-916
We present pollen diagrams and sedimentological analyses from a lake site within an extensive dune system on the Aupouri Peninsula, Northland. Five thousand years ago, a regional Agathis australis–podocarp-broadleaf forest dominated the vegetation,
Autor:
Matt S. McGlone, V. E. Neall
Publikováno v:
New Zealand Journal of Botany. 32:251-269
Pollen diagrams are presented from four lowland Taranaki sites which collectively span the last 13 000 years. Atc. 13000 years ago, lowland Taranaki was occupied by an open grassland in which shrubland was restricted and forest scarce. Beginning c. 1
Autor:
M. Royd Bussell, Brad Pillans
Publikováno v:
Journal of the Royal Society of New Zealand. 22:41-60
Cover beds of a marine terrace, exposed near Fordell, Wanganui district, New Zealand, contain a polleniferous, mostly alluvial sequence, overlying interglacial marine pebbly sand, deposited after the cutting of the Braemore Marine Terrace about 340,0
Autor:
David J. Lowe, Rewi M. Newnham
Publikováno v:
Journal of Quaternary Science. 6:177-193
A 12 000 to 4000 yr BP pollen and tephra-bearing profile from Auckland, New Zealand, provides insights into the vegetation history and evidence for early Holocene volcanic activity in this area centred on the Mount Wellington basaltic volcano. Possib
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