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    Xxx new zealand

    It must, however, be pointed out that these usually contain but little matter of ecological interest, and that for the most part they are lists of plants. Boggy and swampy places also occur near the sea, fed by fresh-water brooks and springs. In both these cases special conditions occur for plantlife, but such, it may be pointed out, are not coastal unless salt be present in excess.In fact, so little has, up to the present time, been published regarding the coastal vegetation of the South Island that I do not consider it necessary to give a summary of our knowledge on the subject. The special factors with regard to coastal vegetation are superabundance of salt in the soil, and high or frequent and prolonged winds.

    Discover your own isolated slice of Kiwi paradise, revel in the birdsong all day long. You are safe, dry and warm, you have a flushing toilet, an awesome shower and a kitchen – while totally surrounded by the best of Pure New Zealand.Properly speaking, the South Island of New Zealand does not form a distinct phytogeographical province. Together with these comes a more equable climate than further inland, so far as extremes of temperature are concerned, but at the same time there is often strong insolation and bright illumination.Strange as it may seem, Cook Strait forms no line of demarcation between the North Island and the South Island floras—so far, at any rate, as the lowland region is concerned. The biotic factor, apart from introduced animals and those concerned in fertilisation, is of little moment, with the exception of the part played by the small land-crabs in the salt meadows, whose innumerable holes must assist materially in aerating the soil, and to some measure, also, in draining the ground.The treatment of the formations, too, will be far from exhaustive. Some attempt, however, will be made to give a word-picture of each formation, and details will he furnished regarding the conditions under which such exists, while something will be said as to the life-forms of the most important constituents. In some places there are distinct traces of ancient shores, and such may contain in large part maritime plants, but unless these are in fairly close proximity to the sea they will not be specially dealt with. As for the actual sea-shore, it may be sandy, rocky, shingly, gravelly, or muddy. Sandy shores merge into dunes, generally of no great height.As in my former phytogeographical papers, the term “formation” is adhered to on the score of priority, At the conclusion of this paper are included, in the Bibliography, the names of the more important papers referring to my subject. As some of the notes, &c., made use of in the preparation of this paper were taken during several voyages in the Government steamer “Hinemoa,” I thank most sincerely the Hon. Gravelly and rocky shores are succeeded by cliffs, stony terraces, gravelly dunes, steep bariks, &c., while muddy stores are frequently the forerunners of salt meadows.

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