My Research Aims, Which Were Not Fulfilled: Crust of Desert Dust Origin
In the last chapter, I reviewed the adventures of my researches in biodeterioration of calcite rocks. I could not be indifferent to phenomena in the natural habitats of my country, the understanding of which, at a basic level, was close to my heart. When I understood one component or another, I urged myself to share the information with others by writing a scientific article in English or a popular article in Hebrew (A reference list is displayed at the end of this chapter).
I was quite close to a superficial understanding of the ecological system that causes east- and south-facing walls in Jerusalem to look brown. I wanted to close the circle of checkups on the biological origin of this coloring. Supported in the fulfillment of my aims by Michael Dvorachek, who operates the scanning electron microscope of the Geological Institute, we made chemical analyses of brown crusts. These were samples from young and old walls in Jerusalem, Masada and near Sede Boqer. The elements spectrum in these different sites was similar and I felt I was on the right track.
I began cooperating with researchers from Seattle, Washington, who specialized in the study of bacteria living on chert stone and rocks in extreme desert areas. The bacteria oxidize iron and manganese oxides derived from air-borne dust. The bacteria fix a thin layer of clay minerals to the chert, thus constructing their microscopic habitats. The result is the dark colored thin layer seen on chert rocks and stones. It was once called “patina” but later, due to confusion in literature “rock varnish” took the lead.
Our scientific article (Hungate et al., 1987) is related to this ecosystem in extreme desert areas. Other people claim that the patina is formed in other ways, however, in my present book I do not have to bring order to everything on earth. When checking walls in Jerusalem I was sure that the hypothesis of drought resistant bacteria fixing desert dust onto limestone walls could be applied here as well. I did not succeed in finding a bacteriologist who was interested in the subject and was ready to solve basic questions arising in this ecosystem. If any of the readers wish to hear my suggestions for research directions and locations – I am here.
A close-up view of the walls of the Mausoleum of Kabakbi showed that the dust accumulation on the wall is protected from rainfall in waves similar to those in Fig. 430. There is a combination here of water flow and transportation of dust and its fixation by microorganisms. I have seen similar waves of moderate water flow on asphalt roads and dirt roads when the transported material was broken pine needles or broken leaves and thin stems. When checking stone pieces that I removed from a site in the Negev Highlands, where dust had accumulated on a construction 4,000 years old, I saw waves on the thin chert layers formed (from dust?) on the limestone. These waves resemble the dust waves on the walls of Jerusalem, but seem to have passed through further development. Fig. 6.16.3 depicts a frozen wave from the Negev Highland; it crosses the entire wide side of the photo.
When it rains, the few drops of water flowing vertically on the stone create a microscopic lake on the horizontal plane between the wave wall and the limestone wall. In the wave seen in Fig. 6.16.4, one can see grains accumulated in that depression. Comparing the grains to the scale bar one may estimate the grains to be 1-2 micron. Let me now tell the whole story that I wished to prove, but did not succeed:
Desert dust transported by winds is deposited constantly over the entire country. In sites where the amount of water is small the dust is not washed away. In these places, e.g., walls all the way from Jerusalem to the Negev Highlands, specialized bacteria fix the dust to the walls through the waves with horizontal components that they construct on the vertical wall. The fixed dust continues to pass through chemical processes at the end of which it becomes a chert layer that preserves the weathering patterns and accumulation that take place on the limestone.
Will my grandson Tomer, who checks the mosses I show him with serious innocence (Fig. 6.16.5), become the one to prove my theory of “wall-browning in Jerusalem”?
A List of Publications Concerning Biodeterioration of Calcareous Rocks
- Danin, A. 1983a. The colors of Jerusalem’s walls. Israel Land and Nature 8: 94-98.
- Danin, A. 1983b. Weathering of limestone in Jerusalem by cyanobacteria. Z. Geomorph. 27: 413-421.
- Danin, A.Gerson, R. and Garty, J. 1983. Weathering patterns of hard limestone and dolomite by endolithic lichens and cyanobacteria: supporting evidence for eolean origin of Terra-Rossa soil. Soil Science 136: 213-217.
- Danin, A. and Garty, J. 1983. Distribution of cyanobacteria and lichens on hillsides of the Negev Highlands and their impact on biogenic weathering. Z. Geomorph. 27: 423-444.
- Danin, A. 1984. Microbial colonization of limestone in the Negev desert. 3rd Int. ACME Symp. Cincinnati, p.10.
- Danin, A. 1985. Palaeoclimates in Israel: evidence from weathering patterns of stones in and near archaeological sites. Bull. Amer. School Orient. Res. 259: 33-43.
- Danin, A. 1986a. Patterns of biogenic weathering as indicators of palaeoclimates in Israel. Proc. Roy. Soc. Edinburgh Biol. Ser. 89B: 243-253.
- Danin, A. 1986b. Patterns of corrosion and abrasion induced by land snails on limestone rocks. Malacol. Rev. 19: 91-98
- Danin, A. 1986c. Habitats of lithobionts on limestone. Israel Society for Microbiology, Jerusalem.
- Danin, A. 1987. Climatic changes in desert areas of Israel as indicated by patterns of biogenic weathering. The 13th Archaeological Congress in Israel, Beer Sheva p.4.
- Hungate, B., Danin, A., Pellerin, N.B., Stemmler, J., Kjellander, P., Adams, J.B. and Staley, J.T. 1987. Characterization of manganese-oxidizing (MnII-MnIV) bacteria from Negev Desert rock varnish: implications in desert varnish formation. Can. J. Microbil. 33: 939-943.
- Danin, A., Wieder, M. and Magaritz, M. 1987. Rhizofossils and root grooves in the Judean Desert and their palaeo- environmental significance. Israel J. Earth-Sci. 36: 91-99.
- Danin, A. 1989a. The use of biogenic weathering of limestone in palaeoclimatic research. In: E. Spanier, Y. Steinberger & M. Luria (eds.) Environmental Quality and cosystem Stability: Vol. V-B: 53-64. ISEEQS Publication, Jerusalem.
- Danin, A. 1989b. Remnants of biogenic weathering as a tool for studying palaeoclimates. Braun-Blanquetia 3(2): 257-262.
- Danin, A. and Caneva, G. 1990. Deterioration of limestone walls in Jerusalem and marble monuments in Rome caused by cyanobacteria and cyanophilous lichens. Biodetereioration International 26: 397-417
- Caneva, G., Gori, E.G. and Danin, A. 1992. Incident rainfall in Rome and its relation to biodeterioration of buildings. Atmospheric Environment 26B (2): 255-259.
- Danin, A. 1992a. Biogenic weathering of marble monuments in Didim, Turkey and in Trajan’s Column, Rome. Proc. 5th Inter. Conf. Envir. Quality and Ecosystem Stability, Jerusalem V/B: 675-681.
- Danin, A. 1992b. Pitting of calcareous rocks by organisms under terrestrial conditions. Israel J. Earth-Sciences 41: 201-207.
- Caneva, G., Gori, E.G. and Danin, A. 1992. Contributo della pioggia battente alla colonizzazione biologica di superfici murarie di Roma Bollettino di Geofisica, CNR-IFA, Roma 15(3): 119-131.
- Caneva, G., Danin, A., Ricci, S. and Conti, C. 1994. The pitting of the Trajan’s column, Rome: An ecological model of its origin. Accademia Nazionale dei Lincei 88: 77-102.
- Danin, A. and Kuenne, I. 1996. A new species of Origanum (Labiatae) from Jordan: O. jordanicum Danin et Kuenne sp.n., and notes on the species of section Campanulaticalyx. Willdenowia 25(2): 601-611.
- Danin, A. 1999. Desert rocks as plant refugia in the Near East. Bot. Rev. 65(2): 93-170.
- Danin, A. 1999b. Sandstone outcrops – a major refugium of Mediterranean flora in the xeric part of Jordan. Israel J. Plant Sci. 47: 179-187.