By John Aitchison
For 20 years John Aitchison has been vacationing the area to movie natural world for the BBC and different broadcasters, taking him to far-away areas on each continent. The Shark and the Albatross is the tale of those trips of discovery, of his encounters with animals and low enterprising participants in distant and occasionally harmful areas. His locations contain the some distance north and the a long way south, expeditions to movie for Frozen Planet and different common background sequence, in Svalbard, Alaska, the distant Atlantic island of South Georgia, and the Antarctic. in addition they surround wild locations in India, China and the USA. In all he unearths and describes key moments within the lives of animals, between them polar bears and penguins, seals and whales, sharks and birds, and wolves and lynxes.
He unearths what occurs behind the curtain and past the digital camera. He explains the practicalities and demanding situations of the filming strategy, and the issues of survival in perilous locations. He files touching moments and dramatic incidents, a few finishing in good fortune, others desperately unhappy. there are occasions whilst a hunted animal triumphs opposed to the chances, and others while, despite training for each final result, catastrophe moves. And, because the writer indicates in numerous incidents that mix nail-biting pressure with hair-raising hilarity, catastrophe can strike for film-makers too.
This is traditional background writing at its best possible, evocative, informative and gripping from first to final.
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Extra info for The Shark and the Albatross: Adventures of a wildlife film-maker
Banded Iron Formations: BIF From the beginning of the Archaean (around 3800 Ma) we find increasing accumulations of a peculiar rock type. BIF or Banded Iron Formations are sedimentary rocks found mainly in sequences older than 1800 Ma. The bands are alternations of iron oxide and chert (Fig. 14), sometimes repeated millions of times in microscopic bands (Fig. 15). 13 This fossil is Primaevifilum, from the Apex Chert in the Warrawoona rocks of Western Australia, dated about 3465 Ma. A photograph down a microscope a) shows a rather blurry outline, which caused unnecessary vicious criticism suggesting that it was not a cell and not a fossil.
A shield of perhaps 10 m (30+ feet) of water might have been needed to prevent damage to a normal early cell by UV radiation. However, the early evolution of the stromatolitic way of life by cyanobacteria may have been a response to UV radiation. With light (and UV) penetrating only a little way into the mat, bacteria were able to live essentially at the foodrich water surface without damage from UV. Cyanobacteria were not just existing at Warrawoona: they were already modifying their microenvironment for survival and success.
0003176 Schopf, J. W. and A. B. Kudryatsev. 2010. A renaissance in studies of ancient life. Geology Today 26: 140–145. Valley, J. W. 2005. A cool early Earth? Scientific American 293 (4): 58–65. pdf Waldbauer, J. R. et al. 2011. Microaerobic steroid biosynthesis and the molecular fossil record of Archean life. PNAS 108: 13409–13414. pdf Questions for Thought, Study, and Discussion 1. Explain the difficulty of finding the age of a rock bed by the fossils in it, and at the same time finding its age by radiometric methods.