Southern hemisphere patterned mires, with emphasis on southern New Zealand
Southern hemisphere patterned mires, with emphasis on southern New Zealand
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南半球的泥沼，重点是新西兰南部
DOI：
10.1080/03014223.1995.9517481
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发表时间：
1995
影响因子：
2.2
通讯作者：
M. McGlone
中科院分区：
文献类型：
--
作者：
A. Mark;P. Johnson;K. Dickinson;M. McGlone
在新西兰南部的山谷头和冰川台阶上的广泛的图案化泥潭：（南纬45° 22 ';海拔1250-1400米），火地岛（54° 53'S; 60-100 m a.s.l.）在凉爽、潮湿的气候条件下形成，有利于泥炭的积累。在新西兰南部的草丛草原景观中，阿帕沼泽池（通常有泥炭岛）和山脊被拉长（池：平均24.5 ± 2.4 m × 7.5 ± 1.0 m），并与缓坡成90°。泥炭深度（0.3-2.5米）最大的下坡边缘的池，有时与基底剖面凹陷。水深达1.3米的沼泽有泥炭基，一般不受地表溪流的补给，也不与地表溪流相连，有陡峭的下坡，有更平缓的上坡，边缘。泥煤可能是初期的（占据小的泥炭洼地），波动的或永久的。在较陡的源头部分，地表和地下渠道连接小溪流池。在冰川台阶上，水池（1公顷）占据了基底岩石凹陷，最多可达1.5米。
Extensive patterned mires in valley heads and on glacial benches in southern New Zealand: (45° 22'S; 1250–1400 m a.s.l.), and valley floors in Tierra del Fuego (54° 53'S; 60–100 m a.s.l.) have developed under cool, moist climatic conditions favourable for peat accumulation. In southern New Zealand's tussock grassland landscape, aapa mire pools (often with peat islands) and ridges, are elongated (pools: mean 24.5 ± 2.4 m × 7.5 ± 1.0 m) and aligned 90° to gentle slopes. Peat depths (0.3–2.5 m) are greatest on downslope margins of pools and sometimes associated with basement profile concavities. Pools up to 1.3 m deep have peat bases, are generally not fed by nor linked to surface streams, and have steep downslope, with more gentle upslope, margins. Pools may be incipient (occupying small peat depressions), fluctuating or permanent. In steeper headwater sections, surface and underground channels link small stream pools. On glacial benches, pools (to 1 ha) occupy basement rock depressions with up to 1.5 m of ...