BEN
BOTANICAL ELECTRONIC NEWS
ISSN 1188-603X


No. 353 November 23, 2005 aceska@telus.net Victoria, B.C.
Dr. A. Ceska, P.O.Box 8546, Victoria, B.C. Canada V8W 3S2

BEN issues 352 and 353 are dedicated
to the memory of

BORIS ALEXANDROVICH YURTSEV

who died in St. Petersburg
on December 14, 2004

BOOK REVIEW: THE LAST GIANT OF BERINGIA

From: David F. Murray [ffdfm@uaf.edu]
O'Neill, Dan. 2004.
The last giant of Beringia: The mystery of the Bering Land Bridge. Westview Press, New York, NY. vii+231 p. ISBN 0- 8133-4197-3 [hard cover] Price: US$26.00/CDN$40.00

Available from:
Westview Press, 387 Park Avenue South, New York, NY 10016
Tel.: (212) 340-8151, Fax: (212) 340-8115
http://www.westviewpress.com/

Those who have delved into Beringian history know the name Dave Hopkins. After an illustrious career with the U.S. Geological Survey, mostly working for the Alaska branch, Dave moved to the University of Alaska Fairbanks as a Distinguished Professor of Quaternary Science. At UAF he was the magnet that attracted faculty and students-botanists, zoologists, geologists, anthropologists, oceanographers-- and the glue that held them together through the activities of the Alaska Quaternary Center.

Dan O'Neill has written a biography of Dave, The last giant of Beringia, the giant referring to Dave, but clearly with a play on the word synonymous with Pleistocene megafauna. Dan has provided background on Dave's upbringing and early years in New Hampshire (born in 1921), the early development of his broad interests in natural history, his education, and on his long and productive professional career of more than 50 years, most of it in Alaska. In recent correspondence I have had with others who worked more closely with Dave and knew him better, I learned that we had each found something in the Dan's account we hadn't known before.

Dan hit the high points of the Bering Land Bridge, its history and impact on our biota, when during glacial intervals Alaska was biologically more an extension of northeast Asia than a part of North America. He described how Dave began to investigate Beringian history, step by step, working with fossil mollusks, sea floor morphology, ancient shorelines, paleosols, beetles, pollen and macrofossils, and the artifacts of early humans. He showed how the results of one study led to another, additively, until a coherent thread had been established. Dave was an intellectual omnivore, the quintessential interdisciplinary scientist, who could seize new ideas from any and all quarters, but when any one of them failed the test, happily discarded it and eagerly move on.

Several important players have smaller parts in the book, and Dan has done justice to the critical influences of botanists, Eric Hult,n and Bob Sigafoos, one archaeologist in particular, Louis Giddings, and many, many others who contributed hugely to Dave's understanding of Beringian paleoecology.

Dave was esteemed by his Russian colleagues just as has Dan described. I took reprints and greetings from Dave to Moscow on one of my trips and met with his old friends who made it abundantly clear that Dave was truly a good friend. Boris Yurtsev was one of those Russian friends. On a visit to Fairbanks, Boris was able to join the annual Quaternary field trip that Dave had instigated as a regular early fall event. We tented overnight on the "green" at Central and then went out to look at Quaternary gravels at local placer mines. Fall color was at its peak and the aspen and birch covered hillsides were a blaze of gold and Boris enchanted.

Dave's work led to symposium volumes to which he contributed papers or ones for which he was the motivating force, the most important of these being the The Bering Land Bridge in 1967 and Paleoecology of Beringia in 1982. More recently in 2001 there appeared a festschrift to Dave, Beringian Paleoenvironments, which is another important synthesis. It was the outcome of a conference that included a very moving evening with Dave, some slides, and his very personal reminiscences. Boris Yurtsev was there with a large Russian contingent, and the paper Boris published in the festschrift is the most complete statement we have of his tundra-steppe concept.

Dave Hopkins died in 2001. Dave's legacy is his family and friends, seminal papers, and lots of colleagues and former students, themselves now important figures in Quaternary science. He was a giant.


PROCEEDINGS FROM THE PANARCTIC FLORA 1998 SYMPOSIUM

Nordal, I. & V. Yu. Razzhivin [eds.] 1999.
The species concept in the high north a Panarctic flora initiative. Det norske videnskaps-akademi. Skrifter. 1. Mat.- naturv. klasse. Ny serie (nr. 38). Oslo. 418 p. ISBN 82-90888-33-3; ISSN 1502- 0096 [soft cover] Price: US$40.00

Limited number of copies is available from:
Inger Nordal [inger.nordal@bio.uio.no]

Thirty-two contributions by US, Canadian, Icelandic, Norwegian, Swedish and Russian botanist deal with problems related to compiling the Panarctic Flora. This Flora would include all the Arctic regions.

The "Panarctic Year" at the Norwegian Centre of Advanced studies was initiated by an international symposium, September 28 to October 3, 1998, with about 30 participants.

Section I in this volume includes the proceedings from this symposium. With the extant knowledge of the history, palaeogeography, evolution, and taxonomy of the Arctic, the editors wanted to be open to different views, and contrasting, even conflicting, views might be found.

During the "Panarctic Year" several workshops (or the so-called "expert group meetings") have been organised on critical genera/families with complicated taxonomy, obviously treated differently within Russian, Nordic, and/or American tradition. The reports from these workshops are presented in Section II and include notes on Cerastium, Draba, Dryas, Papaver, Poaceae, Potentilla, Salix, and Saxifraga.

Section III contains reports on an earlier meeting of the Panarctic Flora committee, zonal subdivision of the Arctic, and an example of a checklist of Arctic members of the Saliaceae family.


A COMPILATION OF ADDITIONS TO THE FLORA OF THE CONTINENTAL PORTIONS OF NORTHWEST TERRITORIES AND NUNAVUT

From: P. M. Catling, W. J. Cody and G. Mitrow, Biodiversity, National Program on Environmental Health, Agriculture and Agri-food Canada, Wm. Saunders Bldg., Central Experimental Farm, Ottawa, Ontario, Canada K1A 0C6 E-mail: [catlingp@agr.gc.ca]

Introduction

The protection of biodiversity in the Canadian north is receiving increasing attention as settlement and exploitation of natural resources expand. Invasive species are rapidly entering the region (Wein et al. 1992, Cody et al. 2000) which includes many native species of concern (Cody 1979, McJannet et al. 1995, Talbot et al. 1999) and many that are important to native people and wildlife (e.g. Marles et al. 2000). A strong and ever growing commitment to the protection of biodiversity is evident in territorial initiatives such as the Northwest Territories Biodiversity Action Plan (NWT Biodiversity Team 2004). With the increasing interest in the protection of natural resources there is an increasing need for accurate information on the flora including particularly the information needed for plant identification. There is also a great international interest in the Canadian portion of the circumpolar flora as a result of cooperative work on classification and evolution of circumpolar plants involving all circumpolar countries. This work also requires that information be current and accessible. The information presented here responds to these needs. The list includes species that are new to the continental areas of Northwest Territories and Nunavut together, and thus new to the classic flora (Porsild and Cody 1980) that covers this region.

The area

In 1980 when the manual of Vascular Plants of the Continental Northwest Territories, Canada (Porsild & Cody 1980) was published the "Territories" included a continental (excluding oceanic islands) land and freshwater area of approximately 3/4 of a million square miles. It extended from the Yukon border north of 60 degrees east to Hudson Bay and was bounded on the north by the Arctic Ocean. On April 1, 1999, the eastern portion of this territory (including all of the District of Keewatin and much of the District of Mackenzie and the District of Franklin) became a part of a separate territory called Nunavut which has a continental area of 350,000 square miles.

Recent work

Since 1980 there have been several regional studies of the flora and vegetation of mainland parts of both Northwest Territories (NT) and Nunavut (NU). Some of these have emphasized phytogeography and included reference to the discovery of additional species ( e.g. Cody et al. 2003) while others have not, often being concerned primarily with detailed information on vegetation composition (e.g. Cody et al. 1984). In addition numerous systematic studies of particular groups of plants have been published and many of these contain additional plant records, i.e. species additional to those included in the manual. To use the guide effectively an update to the information is required. Here we provide the update with an indication of sources of additional information. Since this compilation was prepared two additional sources have become available but the results have not been included here (see Catling 2005 and Catling 2006).

Methods

This compilation includes all additions to the Porsild and Cody (1980) manual known to us and is also based on (1) a literature search in Biosis using such key words as "addition", "Northwest Territories", "new record", "new plant", "flora;" (2) an analysis of the maps in "Flora of the Canadian Arctic Archipelago" (Aiken et al. 2002), (3) a search for additional records in the recently published volumes of Flora of North America (including volumes 2, 3, 4, 22, 23, 25, and 26; (3) a survey of monographs published in Rhodora; and (4) a survey of articles in The Canadian Field-Naturalist. We suspect that with this work we have compiled over 95% of the additions. We will appreciate learning of any that we have overlooked.

This compilation applies only to the combined continental area of NT and NU, i.e. continental N.W.T. in the sense of Porsild and Cody (1980). The northernmost peninsulas of Nunavut, the Boothia Peninsula and the Melville Peininsula, are traditionally not included in the continental area (Porsild & Cody, 1980, p. 2). Additional taxa may include species, subspecies, varieties, forms, hybrids and differentiated races potentially worthy of taxonomic recognition. Additions may result from new discoveries in the area, corrections to existing reports or newly defined taxa.

The taxa are arranged by family and this will help to ensure that users of the 1980 flora are aware of more recently discovered taxa related to those that can be identified using the the 1980 text. More information on these species is available in the references provided.

Synopsis

Porsild and Cody (1980) listed 1113 species. The published additions of 111 taxa listed here includes 94 species, 9 infraspecific taxa (i.e. additional subspecies, varieties and forms of species listed by Porsild & Cody in 1980) and 8 hybrids. Based on the recorded additions and the deletions of 6 species (listed below), 1201 species are known from the combined continental areas of NT and NU. An accurate number of taxa (all categories including different subspecies, varieties, forms and hybrids) is not available at present. Of the additional species, 68 are native and 26 are introduced. The families with the largest representation among the additional species are the grasses (Poaceae) and sedges (Cyperaceae).

Additions to Northwest Territories (NT) and Nunavut (NU)

* = introduced

Acknowledgement

Helpful comments were provided by Dr. Jacques Cayouette.

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