A major contributor to this article appears to have a close connection with its subject.(March 2022) |
Bruce William Hayward | |
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Nationality | New Zealander |
Alma mater | University of Auckland |
Scientific career | |
Fields | Geologist, marine ecology |
Thesis | Lower Miocene geology of the Waitakere Hills, west Auckland, with emphasis on the paleontology (1975) |
Doctoral advisor | Philippa Black, Graham Gibson, Peter Ballance |
Bruce William Hayward MNZM FRSNZ (born 1950) is a New Zealand geologist, marine ecologist, and author. He is known as a leading expert on living and fossil foraminifera. [1]
At the University of Auckland, Bruce W. Hayward graduated in geology with B.Sc. (Hons) in 1971 and Ph.D. in 1975. [2] [3] In 1976–1977 he was a postdoc at the Smithsonian Institution in Washington, D.C. [4] Hayward was from 1978 to 1991 a micropaleontologist for the New Zealand Geological Survey, Lower Hutt. In March 1991 Hayward became the curator of marine invertebrates at the Auckland Institute and Museum, after the retirement of Walter Olivier Cernohorsky. [5] From 1997 to 2002 he was a self-employed research associate in the Geology Department of the University of Auckland, as well as from 1998 to 2000 a James Cook Research Fellow at the University of Auckland. In 2003 he became the Founder and Principal Scientist of Geomarine Research, located in Auckland. He was the Principal Scientist for three Marsden Fund grants: from 2000 to 2002 "Foraminifera and paleoceanography of Bounty Trough, east New Zealand", from 2003 to 2005 "The last global marine extinction: causes and consequences for global biodiversity", and from 2007 to 2010 "Causes of evolution and global extinction in the deep sea". [6] In addition to his research on foraminifera, he has done research on "northern New Zealand geology and landforms, marine invertebrate ecology, industrial archaeology and lichens." [1]
Hayward was from 1980 to 1989 an editor for the Geological Society of New Zealand, from 1988 to 2012 an associate editor for the Journal of Foraminiferal Research, and from 2010 chief editor for Foraminifera, World Register of Marine Species. [6] He is founder and convenor (1984–present) of the New Zealand Geopreservation Inventory and from 1990 to 1993 a member of the New Zealand Conservation Authority and from 1993 to 1996 a member of the Auckland Conservation Board. He co-founded the Offshore Islands Research Group in 1977 and co-founded the Auckland Geology Club in 1993. He is the author or co-author of "over 1000 publications, including more than 280 peer-reviewed papers, hundreds of popular articles, 13 scientific monographs and more than 20 popular books." [1]
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: CS1 maint: postscript (link) The book recounts "the fascinating geological history of the formation of Northland, Auckland and the Coromandel Peninsula and the history of its past animal and plant life." [9] {{cite book}}
: CS1 maint: postscript (link) ebook The Waitākere Ranges is a mountain range in New Zealand. Located in West Auckland between metropolitan Auckland and the Tasman Sea, the ranges and its foothills and coasts comprise some 27,720 hectares of public and private land. The area, traditionally known to Māori as Te Wao Nui o Tiriwa, is of local, regional, and national significance. The Waitākere Ranges includes a chain of hills in the Auckland Region, generally running approximately 25 kilometres (16 mi) from north to south, 25 km west of central Auckland. The ranges are part of the Waitākere Ranges Regional Park.
Anawhata is a beach on the coast of New Zealand west of Auckland.
Whatipu is a remote beach on the west coast of the Auckland Region in the North Island of New Zealand. The Whatipu area has been managed as a scientific reserve by the Auckland Regional Council since 2002. The road to it is unsealed. To the south of Whatipu is Manukau Harbour. To the north is Karekare. Whatipu is located at the southern end of the Waitākere Ranges. Shifting sands have substantially changed the beach since the 1940s. Over 6 square kilometres has been added to the beach since then.
Scenic Drive is a road that runs through the bush-clad Waitākere Ranges from Titirangi to Swanson on the western outskirts of Auckland, New Zealand. It is part of Auckland urban route 24. As the name indicates, it is famous for the sweeping views over the western parts of the Auckland Region.
Huia is a western coastal settlement in West Auckland, New Zealand and forms part of the Waitākere Ranges Regional Park. The majority of houses in Huia are located along Huia Road, which arcs around Huia Bay and heads west towards Little Huia.
Oratia is a semi-rural locality on the western edge of metropolitan West Auckland in New Zealand.
The Auckland Region of New Zealand is built on a basement of greywacke rocks that form many of the islands in the Hauraki Gulf, the Hunua Ranges, and land south of Port Waikato. The Waitākere Ranges in the west are the remains of a large andesitic volcano, and Great Barrier Island was formed by the northern end of the Coromandel Volcanic Zone. The Auckland isthmus and North Shore are composed of Waitemata sandstone and mudstone, and portions of the Northland Allochthon extend as far south as Albany. Little Barrier Island was formed by a relatively isolated andesitic volcano, active around 1 to 3 million years ago.
New Zealand's Northland Region is built upon a basement consisting mainly of greywacke rocks, which are exposed on the eastern side of the peninsula. In-place Eocene coal measures crop out at Kamo, near Whangarei, and Oligocene limestone crops out at Hikurangi, near Whangarei.
Lion Rock is a rocky headland located on Piha Beach in the Waitākere Ranges area of the Auckland Region, New Zealand.
The Āwhitu Peninsula is a long peninsula in the North Island of New Zealand, extending north from the mouth of the Waikato River to the entrance to Manukau Harbour.
John Thomas Diamond was an amateur New Zealand historian and archaeologist. Over 70 years, Diamond documented the industrial, archaeological and social history of West Auckland.
West Auckland is one of the major geographical areas of Auckland, the largest city in New Zealand. Much of the area is dominated by the Waitākere Ranges, the eastern slopes of the Miocene era Waitākere volcano which was upraised from the ocean floor, and now one of the largest regional parks in New Zealand. The metropolitan area of West Auckland developed between the Waitākere Ranges to the west and the upper reaches of the Waitematā Harbour to the east. It covers areas such as Glen Eden, Henderson, Massey and New Lynn.
Little Huia is a western coastal settlement of West Auckland, Auckland, New Zealand and forms part of the Waitākere Ranges Regional Park, bordering the Manukau Harbour. It is located south-west of the settlement of Huia.
Te Toka-Tapu-a-Kupe / Ninepin Rock is an island at the mouth of the Manukau Harbour, at Whatipu in the Waitākere Ranges area.
Paratutae Island, also known as Paratūtai Island, is an island off New Zealand at the mouth of the Manukau Harbour, at Whatipu in the Waitākere Ranges area.
Pukematekeo is a hill in the Waitākere Ranges of the Auckland Region of New Zealand's North Island. It is located west of Henderson, and is the northernmost hill in the Waitākere Ranges Regional Park.
Ruaotuwhenua is a hill in the Waitākere Ranges of the Auckland Region of New Zealand's North Island. At 440-metres, it is one of the tallest of the Waitākere Ranges, and the tallest of the eastern ranges adjacent to Auckland. The peak is the location of an air traffic radome, and a radio mast is located further down the slope of the hill in Waiatarua.
The Waitākere volcano, also known as the Manukau volcano, was a Miocene era volcano that formed off the west coast of the modern Auckland Region of New Zealand's North Island. Erupting intermittently between 23 million and 15 million years ago, the volcano was at one point one of the tallest mountains in New Zealand. The volcano alternated between periods as a seamount and as a volcanic island, before tectonic forces raised the volcano up from the seafloor 17 million years ago. Volcanism at the site ceased 15 million years ago and the cone has mostly eroded, however the modern Waitākere Ranges are formed from the remnants of the volcano's eastern slopes. A number of visible volcanic sites associated with the Waitākere volcano remain around Auckland, including Pukematekeo, Karekare and Lion Rock.
Margaret S. Morley, was a New Zealand malacologist, illustrator and museum curator. A self-trained researcher, Morley joined the Auckland Shell Club in 1980 and became one of the leading experts in the identification of New Zealand micromollusc species. A prolific researcher, Morley published over 119 papers, most of which featured her own illustrations, and in 2004 published A Photographic Guide to Seashells of New Zealand.
Te Rau-o-te-Huia / Mount Donald McLean is a hill in the Waitākere Ranges of the Auckland Region of New Zealand's North Island. It is located to the south of the ranges, near the township of Huia. It is the highest peak of the Waitākere Ranges that borders the Manukau Harbour.