New information on the age and thermal history of a probable Early Triassic siltstone near Kaka Point, South Island, New Zealand

1996 ◽  
Vol 39 (4) ◽  
pp. 581-584 ◽  
Author(s):  
R. K. Paull ◽  
J. D. Campbell ◽  
D. S. Coombs
1999 ◽  
Vol 42 (3) ◽  
pp. 469-488 ◽  
Author(s):  
Asaf Raza ◽  
Roderick W. Brown ◽  
Peter F. Ballance ◽  
Kevin C. Hill ◽  
Peter J. J. Kamp

2020 ◽  
Vol 13 (2) ◽  
pp. 105-125
Author(s):  
Sue McCliskie

More than 3,000 emigrants took up the New Zealand Company's offer of a free or assisted passage to Nelson, the company's Second Colony of New Zealand, from 1841 to 1844 – but did they stay? This article outlines an academic project that combines genealogy techniques and sources with more conventional research, in order to reveal new information about colonial migrants who are often ‘invisible’ in historical accounts. These were predominantly poor English families (with some Germans, Scots and Irish), and they were part of the earliest stages of British colonisation of New Zealand. Genealogy websites such as Ancestry and FamilySearch proved to be central to this research. They provided a gateway to an astonishing amount of information that could ‘locate’ an individual or family, tying them to a certain place, without the researcher knowing which place to look for. This project highlights some of the limitations and dangers of using genealogy methods and sources in academic research – as well as what might be gained. The results suggest that this kind of hybrid methodology incorporating genealogy research can be used successfully within an academic study. In this project, the intricacies of colonial family networks were illuminated, even though the subjects were poor and continued to move around. Surprisingly high levels of mobility were identified, and this was true of women and children as well as men. These findings suggests that using genealogy to trace patterns of colonial mobility is not only important to gain an understanding of individual lives but may also contribute significantly to a better understanding of the larger processes of migration, colonisation and the history of colonial ‘places’.


1999 ◽  
Vol 42 (2) ◽  
pp. 169-188 ◽  
Author(s):  
Asaf Raza ◽  
Roderick W. Brown ◽  
Peter F. Ballance ◽  
Kevin C. Hill ◽  
Peter J. J. Kamp

Paleobiology ◽  
1980 ◽  
Vol 6 (02) ◽  
pp. 146-160 ◽  
Author(s):  
William A. Oliver

The Mesozoic-Cenozoic coral Order Scleractinia has been suggested to have originated or evolved (1) by direct descent from the Paleozoic Order Rugosa or (2) by the development of a skeleton in members of one of the anemone groups that probably have existed throughout Phanerozoic time. In spite of much work on the subject, advocates of the direct descent hypothesis have failed to find convincing evidence of this relationship. Critical points are:(1) Rugosan septal insertion is serial; Scleractinian insertion is cyclic; no intermediate stages have been demonstrated. Apparent intermediates are Scleractinia having bilateral cyclic insertion or teratological Rugosa.(2) There is convincing evidence that the skeletons of many Rugosa were calcitic and none are known to be or to have been aragonitic. In contrast, the skeletons of all living Scleractinia are aragonitic and there is evidence that fossil Scleractinia were aragonitic also. The mineralogic difference is almost certainly due to intrinsic biologic factors.(3) No early Triassic corals of either group are known. This fact is not compelling (by itself) but is important in connection with points 1 and 2, because, given direct descent, both changes took place during this only stage in the history of the two groups in which there are no known corals.


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