TRACE Tree Rings Archaeology Climatology Ecology

More documents

Recommendations

Info

CONTENTS SECTION 1 ECOLOGY A. Bräuning: 8 Tree-ring studies in the Dolpo-Himalya (western Nepal) H. Gärtner and O.U. Bräker: 13 Roots - the hidden key players in estimating the potential of Swiss forests to act as carbon sinks M. Wegst and A. Bräuning: 19 Dendroecological analysis of vegetation dynamics on abandoned heath lands in the Svabian Jura, southern Germany SECTION 2 GEOMORPHOLOGY M. Bollschweiler and M. Ehmisch: 26 Past debris-flow activity from tree-ring analysis at the Bruchji torrent, Valais, Switzerland F. Gussenstätter and A. Bräuning: 31 Changes in growth rates and wood anatomy of broad-leaved and coniferous tree species after a landslide event in the Remstal Valley (Southern Germany) E. Weiss and T. Wils: 36 Tree rings and geomorphological processes in a mountainous region (French Alps) SECTION 3 CLIMATOLOGY J. Block, V.N. Magda and E.A. Vaganov: 46 Temporal and spatial variability of tree-growth in mountain forest steppe in Central Asia D. Frank, J. Esper, U. Büntgen and K. Treydte: 54 The first principal component of a high-elevation ring-width network from the western and central Alps B. Neuwirth and M. Winiger: 58 NAO and Tree Rings - a dendroclimatological network analyses of Central European chronologies U. Sass-Klaassen: 67 Exploring oaks in modern wetland woods in Europe to trace the climate signal in tree-ring series of sub-fossil bog oaks
U. Treter and J. Block: 73 Frost-ring distribution at the upper tree line in Mongolia A. Verstege, J. Esper, B. Neuwirth, M. Alifriqui and D. Frank: 78 On the potential of cedar forest in the Middle Atlas (Morocco) for climate reconstructions U. Büntgen, J. Esper, M. Schmidhalter, D. Frank, K. Treydte, B. Neuwirth and M. Winiger: 85 Using recent and historical larch wood to build a 1300-year Valais-chronology SECTION 4 ISOTOPES AND CLIMATE I. Poole, U. Sass-Klaassen, T. Wils, G. Helle, G. H. Schleser and P.F. van Bergen: 94 The use of stable-isotope dendrochronology for environmental interpretations from tree-ring patterns in sub-fossil bog oaks K. Treydte, C. Welscher, G.H. Schleser, G. Helle, J. Esper, M. Winiger, D. Frank and U. Buentgen: 100 The climatic signal in oxygen isotopes of junipers at the lower timberline in the Karakorum, Pakistan G. Helle, K. Treydte & A. Verheyden: 107 Tropical Swietenia macrophylla wood reveals a systematic recurring carbon isotope pattern SECTION 5 PALAEO-ENVIRONMENTS U. Sass-Klaassen, M. Kooistra, L. Kooistra, E. Hanraets, P. van Rijn and H.-H Leuschner: 112 How did bog oaks grow? Excavation of a past woodland at Zwolle-Stadshagen, The Netherlands SECTION 6 CULTURAL HERITAGE N. Bleicher: 118 Great efforts on small woods. Analysis of short ring-series from the neolithic lakeshore settlement of Hornstaad-Hörnle I A S. van Daalen & J. van der Beek: 123 Dendroprovenancing ship’s timbers. A pilot study on a Dutch 18th century ‘ventjager’ E. Jansma and E. Hanraets: 131 Dating Flanders - towards a Flemish tree-ring chronology of oak E. Jansma, E. Hanraets and T. Vernimmen: 139 Tree-ring research on Dutch and Flemish art and furniture
Page 1 and 2: Forschungszentrum Jülich in der He
Page 3 and 4: Schriften des Forschungszentrums J
Page 5 and 6: Bibliographic information published
Page 10: T. Vernimmen and U. Sass-Klaassen:
Page 13 and 14: Tree-ring studies in the Dolpo-Hima
Page 15 and 16: Rara MLD (Abies) Rara RW (Abies) Ts
Page 17 and 18: Cook, E.R., Krusic, P.J. & P.D. Jon
Page 19 and 20: Material and methods In the first p
Page 21 and 22: Correlations for all trees (no site
Page 23 and 24: Acknowledgements The authors wish t
Page 25 and 26: Results and interpretation Species
Page 27 and 28: Figure 3: Multitemporal maps of est
Page 30 and 31: SECTION 2 GEOMORPHOLOGY
Page 32 and 33: Zurich Geneva Study site Zermatt Fi
Page 34 and 35: lot of debris-flow events can be se
Page 36 and 37: Changes in growth rates and wood an
Page 38 and 39: Growth reductions and eccentricity
Page 40 and 41: 40% of all trees in the landslide a
Page 42 and 43: Figure 1: Location of study areas H
Page 44 and 45: Ai− rBi Eccentricity for year i i
Page 46 and 47: The event frequency per year for th
Page 48: Shroder, J.F. (1980): Dendrogeomorp
Page 51 and 52: Temporal and spatial variability of
Page 53 and 54: 120 100 80 (Dlink/Dmax)*100 60 Uppe
Page 55 and 56: Figure 6: Results of stepwise clust
Page 57 and 58:
Figure 8: Forest types and forest d
Page 59 and 60:
The first principal component of a
Page 61 and 62:
Figure 2: Correlations of the 1 st
Page 63 and 64:
NAO and Tree Rings - A dendroclimat
Page 65 and 66:
5°E 10°E 15°E 50°N 45°N Figure
Page 67 and 68:
The smaller bars show the number of
Page 69 and 70:
a b c d Significant correlating are
Page 71 and 72:
Neuwirth, B., Esper, J., Schweingru
Page 73 and 74:
Unterspreewald,Brandenburg,Germany
Page 75 and 76:
Unterspreewald, Brandenburg, German
Page 77 and 78:
Leuschner, H.H., Delorme A. & H.-C.
Page 79 and 80:
Figure 1: Location of the monitorin
Page 81 and 82:
Figure 3: Examples of the distribut
Page 83 and 84:
On the potential of cedar forests i
Page 85 and 86:
At every site, two cores per tree w
Page 87 and 88:
Maximum replications are reached in
Page 89 and 90:
Schweingruber, F.H., Eckstein, D.,
Page 91 and 92:
developed that can be used to study
Page 93 and 94:
4 3 2 1 0 -1 -2 normalized Schmidha
Page 95 and 96:
This value is based on the fact tha
Page 97 and 98:
Stokes, M.A. & T.L. Smiley (1968):
Page 99 and 100:
The use of stable isotope dendrochr
Page 101 and 102:
3.0 2.5 Z74 2.0 1.5 1.0 0.5 0.0 3.0
Page 103 and 104:
Conclusions The combined stable car
Page 105 and 106:
The climatic signal in oxygen isoto
Page 107 and 108:
Results Figure 2 shows the raw ring
Page 109 and 110:
Secondly, the records are short and
Page 111 and 112:
Jouzel, J., Hoffmann, G., Koster, R
Page 113 and 114:
Although the difference between min
Page 116 and 117:
SECTION 5 PALAEO-ENVIRONMENTS
Page 118 and 119:
Results and discussion Of 59 oaks a
Page 120:
Acknowledgements This research was
Page 123 and 124:
Great efforts on small woods Analys
Page 125 and 126:
Some 250 of them - mainly beeches (
Page 127 and 128:
References Billamboz ,A. (1990): Da
Page 129 and 130:
coefficient can be expected from in
Page 131 and 132:
country region covered by theCATRAS
Page 133 and 134:
Figure 2: Map of the Netherlands an
Page 135 and 136:
Jansma, E., Sass-Klaassen, U., de V
Page 137 and 138:
The aim of the current study is to
Page 139 and 140:
Figure 1: Map of archaeological sit
Page 141 and 142:
0.8 correlation coefficient (r) 0.4
Page 143 and 144:
Acknowledgements We would like to e
Page 145 and 146:
Figure 2: 17th century forgery (Mus
Page 147 and 148:
1400 1450 1500 1550 1600 1650 1700
Page 149 and 150:
Table 2 - Average annual-growth ind
Page 151 and 152:
Conclusion The data set we studied
Page 153 and 154:
Figure 1: Collapsed foundation (Pho
Page 155 and 156:
A list of the archaeological sites
Page 157 and 158:
personal communication) believe tha
Page 159 and 160:
Table 4: Success rates of the dendr
Page 161 and 162:
wood with no strong common tree-rin
Page 163 and 164:
Jansma, E. (1996): An 1100-Year Tre
Page 165 and 166:
Malacochronology, the application o
Page 167 and 168:
Fladen Grounds 100 m Norway 30 m UK
Page 169 and 170:
higher with the chronology of growt
Page 171 and 172:
0 140 200 growth index 120 100 80 6
Page 173 and 174:
an underlying mechanism but demonst
Page 175 and 176:
Witbaard, R., Jenness, M.I., Van de
Page 177 and 178:
TRACE 2003 Utrecht (NL) 1 st -3 rd
Page 179 and 180:
TRACE 2003 Utrecht (NL) 1 st -3 rd
Page 181 and 182:
Schriften des Forschungszentrums J
Page 183 and 184:
Page 185 and 186:
Page 187:
Forschungszentrum Jülich in der He
show all

TRACE Tree Rings Archaeology Climatology Ecology

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?