
Fifteen million years ago, Central Otago was a lake. We know this because the mud, sand and gravel dumped into this lake from the surrounding hills are piled high under the golden tussock and savory scrub of Southland range. Ever since Lake Manuherikia dried up, its dry muck bottoms have been hosed down by every storm that manages to get past Fiordland into the dry rainshadow of the Southern Alps. Each downpour washes the gullies and swirls new tunnels and holes into the soft sediment. Since the Oligocene, the mountains have grown higher and higher until glaciers clung to the tops and crept to the valleys. Relentless grinding by ice turns any solid rock into a heap of pulverized dust the consistency of flour. The wild wind hauls it easily, and piles can accumulate miles away wherever the air slows enough to drop its load. The Germans named this phenomenon first, and we use the term 'loess' (read: luss) for deposits milled by glaciers and sorted by wind.

Until 800 years ago, outlandish birds trotted around New Zealand. That's not to say they don't anymore, it's just that they're so much smaller now. The Giant Moa of Southland stood at twelve feet. It was here, busy grazing during the Norman invasion of England. None are now alive, but Otago is littered with the record of flightless giants and the flying predators that ate them. Lake Manuherikia left the means to save the bones of bird and beast long enough for us to make educated guesses about life in the relatively recent past.

Huge three-toed golem-like grazers with heads smaller than your average chihuahua aren't the smartest animals in the zoo, so it's not surprising that the hundreds of old potholes in Lake Manuherikia sediment contain more than a few Giant Moa skeletons, extinct Kiwi femurs, and Haast Eagle claws. Every time a wandering bird died in the treacherous booby-trapped terrain, it was covered by windblown loess and rain-washed mud. Some skeletons were buried so quickly that they are still assembled correctly. The process is still happening every season, trapping modern mammals, sheep and rabbits together with the ancient forms they have replaced (with the help of human colonizers). Each storm that passes acts as a bulldozer, trencher, and industrial blender all in one - resulting in such confusion of the strata that ancient and modern bones are juxtaposed in unlikely ways.
So maybe I can be excused for spending an hour exposing a rabbit that died five years ago - my vertebrate anatomy suffered from overexcitement, and I realized only too late that my prize had huge front teeth, quite unlike a bird. But we discovered other clues as we poked along on Ray Bell's ranch. We got the idea from a PhD student in Dunedin, Jamie Wood, who directed us to Chatto Creek. Carey Donald joined us for a long weekend holiday from her research in Australia, and we wound through the Otago hills until we saw Jamie's landmark: a lot of old cars and a bridge. That's how we wandered into Mr. Bell's front yard.



PS: this computer is so slow, it won't upload the rest of my sweet pictures. you'll just have to wait. our customer service representative is Helen Wait. if you have complaints, go to Helen Wait.