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Net Werk voor de Geschiedenis van Hygiëne en Milieu, 1994-1996 ...

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spread of Man<strong>de</strong> culture from the<br />

S<strong>en</strong>egal-Niger River region to areas<br />

closer to the emerging networks<br />

of coastal tra<strong>de</strong> further south and<br />

west.<br />

David Lee Scho<strong>en</strong>brun<br />

<br />

becomm<strong>en</strong>tarieert:<br />

Brooks’ Landlords and Strangers<br />

does not closely argue the evi<strong>de</strong>nce<br />

for pre-colonial <strong>en</strong>vironm<strong>en</strong>tal<br />

change in the extreme western portion<br />

of greater West Africa. He does<br />

so in Western Africa to c. 1860<br />

A.D.; A Provisional Historical<br />

Schema Based on Climate Periods.<br />

Indiana University African Studies<br />

Program Working Papers Series No.<br />

1. An article in Cahiers d’étu<strong>de</strong>s<br />

africaines (1986) synthesizes the<br />

earlier synthesis.<br />

Th e authority on historical evi<strong>de</strong>nce<br />

most likely remains Sharon Nicholson,<br />

“A Climatic Chronology<br />

for Africa: Synthesis of Geological,<br />

Historical, and Meteorological Information<br />

and Data.” Unpublished<br />

Ph.D. Dissertation, University of<br />

Wisconsin, Madison, 1976. In<br />

lieu of the diss, try her article in<br />

Jour. of Afr. Hist. 20,1 (1979), 31-<br />

49. More and more realiable data<br />

come from various archaeological<br />

and paleo<strong>en</strong>vironm<strong>en</strong>tal teams of<br />

researchers. Try Jean Devisse (ed.)<br />

Vallees du Niger (Paris: Reunion<br />

<strong>de</strong>s Musées Nationaux, 1993)<br />

[Reviewed by J Vansina in curr<strong>en</strong>t<br />

number of JAH].<br />

12/13<br />

For more rec<strong>en</strong>t eras the material<br />

thick<strong>en</strong>s up rapidly.<br />

James Webb gaat dieper in op het<br />

thema:<br />

In Desert Frontier: Ecological<br />

and Economic Change Along the<br />

Western Sahel, 1600-1850 (Univ.<br />

of Wisconsin Press: Madison, WI,<br />

1995), I examined the historical<br />

evi<strong>de</strong>nce for climatological change<br />

in the western Sahel. I found that<br />

the historical evi<strong>de</strong>nce strongly suggested<br />

a long-term tr<strong>en</strong>d toward increasing<br />

aridity which began in the<br />

late-sixte<strong>en</strong>th or early sev<strong>en</strong>te<strong>en</strong>th<br />

c<strong>en</strong>tury and continued throughout<br />

the period of study<br />

Desert Frontier might be read<br />

as broadly supportive of George<br />

Brooks’ periodization of climate<br />

change for western Africa, summarized<br />

most rec<strong>en</strong>tly in Landlords<br />

and Strangers (1992). In it he argued<br />

for a “wet” phase from c.1500<br />

to c.1630, a “dry” phase from c.<br />

1630 to c.1860, and a “wet” phase<br />

from c.1860 to c.1900. Desert<br />

Frontier thus does not support the<br />

periodization ad<strong>van</strong>ced by Sharon<br />

Nicholson, who argued for a “wet”<br />

period from the late-fi fte<strong>en</strong>th to<br />

the late-eighte<strong>en</strong>th c<strong>en</strong>tury. But<br />

Desert Frontier also argues that the<br />

sev<strong>en</strong>te<strong>en</strong>th and eighte<strong>en</strong>th c<strong>en</strong>turies<br />

were more humid than the<br />

ninete<strong>en</strong>th or tw<strong>en</strong>tieth c<strong>en</strong>turies,<br />

and thus that the i<strong>de</strong>a of “wet” and<br />

“dry” phases which suggests oscillation<br />

around a long-term stable<br />

12<br />

13<br />

50<br />

650-651<br />

contactblad <strong>van</strong> <strong>de</strong><br />

stichting net werk <strong>voor</strong> <strong>de</strong><br />

geschie<strong>de</strong>nis <strong>van</strong> hygiëne <strong>en</strong> milieu<br />

redactie: myriam d a r u<br />

webversie: jan <strong>van</strong> <strong>de</strong>n n o o r t<br />

<strong>Net</strong> <strong>Werk</strong> 50 - maart <strong>1996</strong><br />

mean obscures the fact that there<br />

was a long-term tr<strong>en</strong>d toward increasing<br />

aridity which characterized<br />

the period c.1600 to the pres<strong>en</strong>t.<br />

Desert Frontier argues that during<br />

the period 1600-1850 the<br />

long-term tr<strong>en</strong>d toward increasing<br />

aridity had a profound impact on<br />

both farming and herding peoples.<br />

In broad overview, the increasing<br />

aridity caused the expansion of the<br />

great camel zone, pushed the Sahelian<br />

cattle zone ever farther to the<br />

south, and rolled back the zone of<br />

rainfed agriculture. Th e <strong>de</strong>sertifi cation<br />

of the Sahel provoked transformations<br />

in ways of life. Early in this<br />

period, a new ethnic i<strong>de</strong>ntity, that<br />

of the “Whites” (Arabic: al-Bidan),<br />

was forged. Th e emerg<strong>en</strong>ce of this<br />

<strong>de</strong>sert-edge i<strong>de</strong>ntity was the result<br />

of many transformations in i<strong>de</strong>ntity<br />

among formerly Arab, Berber,<br />

Wolof, Soninke, Fuutanke, and<br />

Bafur groups. Th e <strong>de</strong>siccation of the<br />

<strong>de</strong>sert edge was accompanied by an<br />

increase in political viol<strong>en</strong>ce wh<strong>en</strong><br />

competition for scarcer resources<br />

int<strong>en</strong>sifi ed and new economic patterns<br />

came into being.<br />

In my original post on H-ASEH<br />

, I also<br />

m<strong>en</strong>tioned horse cavalry in the<br />

sahel in response to a post from<br />

W.M. Reger IV, a Russianist working<br />

on the Russian army, who was<br />

inquiring after other work on sev<strong>en</strong>te<strong>en</strong>th-c<strong>en</strong>tury<br />

<strong>en</strong>vironm<strong>en</strong>tal<br />

history and the impact of warfare<br />

and cavalry in specifi c. My work<br />

on Sahelian horse cavalry (fi rst<br />

published in the Journal of African<br />

History, vol. 34, no.2 (1993)) argues<br />

for a horse-slave cycle which<br />

s<strong>en</strong>t Black African slaves north both<br />

into the <strong>de</strong>sert and to the Maghrib<br />

in exchange for horses from North<br />

Africa and horses bred along into<br />

the sa<strong>van</strong>na suff ered high mortality;<br />

they were used for military purposes<br />

which produced more slaves for<br />

export to both (1) Atlantic and (2)<br />

Saharan and North African markets.<br />

(For a rec<strong>en</strong>t overview of the<br />

rec<strong>en</strong>t literature on horse cavalry,<br />

see Robin Law, “Th e Horse in Pre-<br />

Colonial West Africa,” in Cavalieri<br />

Dell’Africa (C<strong>en</strong>tro Studi Archeologia<br />

Africana: Milan, 1995), 175-<br />

184.)<br />

Gro<strong>en</strong> imperialisme<br />

Richard H. Grove, Gre<strong>en</strong> Imperialism:<br />

Colonial Expansion, Tropical<br />

Island E<strong>de</strong>ns and the Origins of Environm<strong>en</strong>talism,<br />

1600-1860 (Cambridge<br />

University Press, Cambridge,<br />

1995), xiv + 525 pp., ISBN 0 521<br />

40385 5.<br />

Besprok<strong>en</strong> door Jane Carruthers,<br />

University of South Africa<br />

From its inception as a distinct<br />

branch of historical <strong>en</strong><strong>de</strong>avour,<br />

<strong>en</strong>vironm<strong>en</strong>tal history has be<strong>en</strong><br />

dominated by the United States.<br />

Th e publications emanating from<br />

13/14<br />

13<br />

14

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