The Palaeohydrology of the Late Pleistocene Lake Tauca on the Bolivian Altiplano and Recent Climatic Fluctuations

The Palaeohydrology of the Late Pleistocene Lake Tauca on the Bolivian Altiplano and Recent Climatic Fluctuations

Sonderdrucke aus der Albert-Ludwigs-Universität Freiburg ALBRECHT KESSLER The palaeohydrology of the Late Pleistocene Lake Tauca on the Bolivian Altiplano and recent climatic fluctuations Originalbeitrag erschienen in: J. C. Vogel (Hrsg.): Late Cainozoic palaeoclimates of the Southern Hemisphere : proceedings of an international symposium held by the South African Society for Quaternary Research in Swaziland, 29 August - 2 September 1983. Rotterdam [u.a.]: Balkema, 1984, S. 115 - 122 SASQUA Intrntnl Sp Szlnd 2 At 2 Sptbr 8 The palaeohydrology of the Late Pleistocene Lake Tauca on the Bolivian Altiplano and recent climatic fluctuations AEC KESSE Unvrttt rbr, Grn ASAC. Appln, th tr bdt t th plhdrl f th t ltn (2 00 000 n th Altpln (Sth Arn And, vrl r dd t h h th lt ndtn t hv hnd n prn th th rnt lt n rdr t th frtn f th pll pbl. It hn tht prpttn t hv nrd b t lt 0 % n th ntr Altplnbn n prn th tht f td. h xpl f th rnt tr bdt flttn f t h tht th nd tn drn th prd n bt b xplnd b thrd hft f th tphr rltn blt n th r f th Alt pln. IOUCIO h rvnlvn Altpln ld tprph dprn (. Sn th nrthrn prt hhr nd ttr, t drnd fr nrth t th b th dr rvr hh fl nt ld l, th p. d th thrn Altpln l nld th Slr f Cp nd Un. h nvttn b Srvnt nd nt (8 hd tht thr ltrn trnrn hv rrd n th Mddl ltn, hh ntd th thr bn t fr lr l. h ll , th lt n, frd n th t ltn btn 2 00 nd 000 . It vrd 4 000 2 nd hd xl dpth f 60 . bt 0 000 hd bn rdd t pprxtl th z f p. rn th ln thr r nl ll flt tn f th l lvl. Klr (66 rprtd n rnt vrtn nd th frtn f n l (UrUr n th thrn Altpln. Mrr nd l ( r bl t prv tht th t Gl tn n th Crdllr d lnt nd th Ql p n th r f th nrthrn Altpln lntd t btn bt 28 000 nd 4 000 . A rthr nr rdvn f th Ql p n prr bt 00 nd lntd bt 000 (nn II rn. 0 000 t hrdl, f t ll, lrr thn t td. h n ln dprn drn th nn II rdvn prbbl nt r thn 00 . Evdn f t ltn lr dvn h l bn fnd n thr prt f th Altpln thnt r (Crdllr d Aplbb, • br (82 Crdllr l, 0. h nn II rdvn n l b prd th th xn tp prfl brvd n th C r f t Antrt (r t l. h r hrnl ndt rltvl ld prd fr 000 t 000 . h flln rntrtn f th lt drn th nn II rdvn n th tr bdt tn fr . h lthd h lrd bn ttd n nr ld l (.. b pld Sndr nd nbn 62 Klr 6 Grv nd lln 6 d 6 Gll 0 tzr t l. Ktzbh 80 ). Sn lrd xtd drn th nn II rdvn, t prn drn th prd nnt b xplnd b n ddtnl rnff fr ltn lr f th bn. It rn t b d t hn n vprtn ndr prpttn. In n t rr bl tht drn th ll rtrt fr ptn nn II t p tn nn I btn 000 nd 0 000 drd t dpt bn ddtnll fd b ltn lr drn th prd. QUAIAIE ESIMAES O AS EAOAIO A ECIIAIO O E AAEOAKE AUCAEIO In rdr t llt th tr bdt f ll , th Alt pln dvdd nt vrl r (. nd bl . h fr fr th rnt ttn r fr Klr (6, 0 nd Klr nd Mnh (68. r . t ltn nd th Altpln (r, l v rdn t Srvnt nd nt (8. 6 bl . hdrll nd ltll dt f th Altpln. Ar nt nt pr. rnff (km') (r ffnt Ar f nrthrn 22 00 0. Ar f thrn 20 00 0.b Cthnt r f tht thnt r f dr rvr 00 0.22 0.0 Cthnt r f dr rvr tht thnt r f t 0 20 0.4 0.0 Ar f t (t ltn 00 0. Cthnt r f t (t ltn 48 400 0. 0.2 h n nnl tr bdt f ld l t lbr n b xprd b th tn C E = ° hr L th nnl prpttn nt th l, th n ttl nnl rnff fr th thnt r nd E th n nnl l vprtn. In th vr td th nr n rnff fr th thnt r hh rrd tthr th dr n vptrnprtn d t tprtr dprn, lltd th th tr bdt tn f th thnt r: Rc = Pc Ec hr th nnl prpttn nt th thnt r, EC th nnl vptrnprtn fr th thnt r. Ardn t dr b Wndt ( th nr n rnff hn th prpttn nt th thnt r nr pl n nr n rltv hdt (U f th r n th bn (bl 2. bl 2. h hn n th rnff ffnt K = c /Pc dpndnt n prpttn nt th bn c (rdn t Wndt . (r 20 0 40 0 60 0 80 0 00 0 20 0 0.00 0. 0.20 0.26 0. 0.6 0.40 0.40 0.40 0.0 0.0 0.600 Evprtn fr th l nd t hn dpndnt n th rf tprtr nd rltv hdt f th r lltd th n rdn bl frl: E = f((Q = f((Q hr ntnt, f( fntn f th nd vlt, Q th vpr prr t th tr rf nd th vpr prr 117 f r. h dr n vptrnprtn f th thnt r th dr n tprtr lltd n th ftr th vprtn fr th l rf. r ttn th rnt l vprtn f th Altpln th vl fr t d, nl E = .48 ( pr r. t n th thrn Altpln drr, E prbbl ht hhr. r th rn th flln lltn rprnt th nl ndtn fr n nr n prpttn. h xl tprtr dprn fr th nn II rdvn (= ° C lltd fr th n ln dprn (00 nd th tprtr rdnt f th r nr th rnd (0.80. ° C00 , rdn t Klr 6. ESUS O E CACUAIOS h flln ndvdl ll dntrt th ntvt f th dl. bl h ht prnt f th nnl tr ppl ld b rprntd b th prpttn nt (A, th rnff fr th thnt tht dhr fr t (, nd th dhr fr t (C n h . C : A = 0, AE = 0, A = O. Wht ld hv hppnd f th ll hd bn bjt t td lt ndtn, tht , f hn n prpttn, vprtn nd tprtr hd nt rrd? Or lltn h tht th l ld hv drd p n bt 0 r. In th xpl th prpttn nt th p 2% (bl . C 2: A 0, AE = 0. h nd tn : h h t th prpttn n th ntr bn b nrd n prn th td ndtn fr th ll t xt? h nnl prpttn nt ld hv t b nrd b 8% ll vr th thnt r. A bl h, th dhr fr t ld thn ppl 0% f th tr fr . C : AE 0, A 0, A = 0. A lrd ntnd, tprtr dr f ° C n b ddd fr th n ln dprn drn th nn II rdvn. h ndt dr n vprtn f 8% n prn th th t tn td. It n l b d tht prpttn nd rltv hdt hv nt hnd. h t tht th xtn f th ll nt rd. It ld dppr n bt 00 r. h tr ppl f th ll ld b rltvl ll dtrbtd n ll thr pnnt. C 4: AE 0, A 0, A O. h bd n th ndtn n . h dft pntd b n nr n prpttn. In th f dr n vprtn b 8% d t th tprtr, prpttn n th ntr bn t b nrd b 40% n rdr t rnt th xt n f th ll . 8 C : A 0, A 0, A 0, Ad 0 (. In lltn 4 t nt nt tht th prpttn r n nr n th rltv hdt f th r l t th rnd ( n th thnt r. In rdr t hhtn th nl ndtn fr pbl nr n prpttn t ll l b d tht th rltv hdt vr th rf nrd b % prd th td ndtn. n th tprtr hn nt ndrtn th ld n dr n E b ttl f 2%. h nr nr n prpttn (A ld thn tll b h 0%. bl . Mn nnl tr ppl fr th ll n prnt. A rpttn nt nff fr th thnt tht dhr fr t C hr f t A C 2 4 4 C 2 2 8 0 C 39 26 35 C 4 2 2 46 C 0 24 46 h rlt n b rzd fll: h xtn f th ll nnt b xplnd tht n n nr n prpttn f t lt 0% n th ntr bn. Althh th dhr fr t f ndr prtn fr th tr bdt f th thrn Altpln td, t pld vr prtnt rl drn th t ltn fr th ll (bl , . EECIOS AOU E AAEOCIMAE It h bn pntd t rptdl (.. n 8 lhn 8 Mrr 8 Slnr 8 Strtrrtt nd brt 8 tht drn th prd fr 8 000 nd 400 (Sthrn phr thrl x thr n nl r n tprtr n th t hphr.

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