A palynological study of Polynesian and European effects on vegetation in Coromandel, New Zealand, showing the variability between four records from a single swamp

被引:20
作者
Byrami, M
Ogden, J
Horrocks, M
Deng, Y
Shane, P
Palmer, J
机构
[1] Univ Auckland, Sch Geog & Environm Sci, Auckland 1, New Zealand
[2] Univ Auckland, Ctr Archaeol Res, Auckland 1, New Zealand
[3] Univ Auckland, Dept Geol, Auckland 1, New Zealand
[4] Queens Univ Belfast, Sch Archaeol & Palaecoecol, Belfast BT7 1NN, Antrim, North Ireland
关键词
palynology; charcoal; Pteridium; deforestation; Kaharoa Tephra; Kauaeranga; Coromandel; New Zealand;
D O I
10.1080/03014223.2002.9517706
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Seven cores were extracted from a river terrace swamp in the forested Kauaeranga valley, Coromandel Peninsula, New Zealand. High-resolution (c. 36-73 yr interval) pollen records were obtained from four of the cores and aged by radiocarbon dating and with stratigraphic reference to the 665 +/- 15 C-14 yr BP Kaharoa Tephra. The records span the last c. 1800 yr and show that the vegetation consisted of lowland podocarp-hardwood forest before deforestation by burning occurred. The pattern of deforestation at Kauaeranga, indicated by the abrupt dominance of Pteridium with concurrent increased charcoal, is typical of pollen records associated with early Polynesian settlement in New Zealand. Peaks of Pteridium and charcoal were also found in sediments deposited after European settlement. Different cores show marked palynological and stratigraphic differences relative to the Kaharoa Tephra, most importantly with regard to the timing of deforestation. Deforestation occurred close to the Kaharoa, at a calculated age of c. 750 BP in one core but well above the Kaharoa (c. 480 BP) in another. The stratigraphic unconformities between cores are attributed to variable fluvial processes causing an uneven deposition of sediments within the swamp.
引用
收藏
页码:507 / 531
页数:25
相关论文
共 32 条
[1]  
Allan H.H., 1961, FLORA NZ, V1
[2]  
Brownsey P., 1989, NZ FERNS ALLIED PLAN
[3]  
CLARK R L, 1982, Pollen et Spores, V24, P523
[4]   NAME CHANGES IN THE INDIGENOUS NEW-ZEALAND FLORA, 1960-1986 AND NOMINA NOVA .4. 1983-1986 [J].
CONNOR, HE ;
EDGAR, E .
NEW ZEALAND JOURNAL OF BOTANY, 1987, 25 (01) :115-170
[5]  
CRANWELL LM, 1953, AUCKLAND I MUSEUM B, V3
[6]   A REVIEW OF LATE QUATERNARY SILICIC AND SOME OTHER TEPHRA FORMATIONS FROM NEW-ZEALAND - THEIR STRATIGRAPHY, NOMENCLATURE, DISTRIBUTION, VOLUME, AND AGE [J].
FROGGATT, PC ;
LOWE, DJ .
NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS, 1990, 33 (01) :89-109
[7]  
HAYWARD B W, 1974, Journal of the Royal Society of New Zealand, V4, P161
[8]  
HAYWARD BW, 1978, KAUAERANGA KAURI PIC
[9]   High spatial resolution of pollen and charcoal in relation to the c600-year-BP Kaharoa Tephra: Implications for Polynesian settlement of Great Barrier Island, Northern New Zealand [J].
Horrocks, M ;
Deng, Y ;
Ogden, J ;
Alloway, BV ;
Nichol, SL ;
Sutton, DG .
JOURNAL OF ARCHAEOLOGICAL SCIENCE, 2001, 28 (02) :153-168
[10]  
Krzywinski, 1989, J BIOGEOGR