Thinking Molecularly, Anything Goes: From Mummies to Oil Spills, Doubts to New Directions

Author(s):  
Susan M. Gaines ◽  
Geoffrey Eglinton ◽  
Jürgen Rullkötter

Though the biomarker saga began with attempts to understand the ancient provenance of petroleum and with the concept of “fossil molecules” and search for early forms of life, the explorations of the past 50 years have led organic geochemists far afield of these first endeavors. As Geoff and Max Blumer recognized back in the 1960s, and as microbiologists began to realize in the early 1980s, the usefulness of the biomarker concept is not restricted to geologic time. Most organic geochemists have, at one time or another, applied their techniques and expertise to the resolution of environmental problems, or found a way to address some archaeological mystery. One of the Bristol group’s most vibrant research programs now has its chemists brushing shoulders not with geologists and oceanographers, but with archaeologists and anthropologists concerned with the evolution of human civilizations and societies. Much of the impetus for the application of biomarker concepts to archaeologists’ questions in the 1970s and 1980s came from petroleum geochemists, not least from Arie Nissenbaum, a geochemist at Israel’s Weizmann Institute of Science who developed a keen interest in the role that geological events and circumstance might have played in the history of civilizations in the Fertile Crescent region. Nissenbaum was fascinated by the bizarre geology and chemistry of the Dead Sea Basin area, where oil seeps and impressive raftlike chunks of asphalt floating on the surface of the lake had long tempted oil prospectors to no avail. Renewed interest in the area’s oil potential in the early 1980s attracted a wave of geochemical studies, and Israeli geochemists scrambled for laboratory resources and funding from abroad. Jürgen, still with Dietrich Welte’s group, did a detailed biomarker study at the behest of an Israeli colleague, and when Nissenbaum saw the results he suggested to Jürgen that they apply Jülich’s considerable GC-MS capability to solving an entirely different sort of mystery. Excavations of archaeological sites in the vicinity of the Dead Sea had turned up solid chunks of black, sticky material that was used as early as 3000 B.C., either in materials used for construction or as a glue to attach tool heads to wooden handles.

1992 ◽  
Vol 38 (3) ◽  
pp. 292-304 ◽  
Author(s):  
Aaron Kaufman ◽  
Yoseph Yechieli ◽  
Michael Gardosh

AbstractThe Dead Sea is surrounded by chemical and detrital sediments that were deposited in its larger precursor lakes, Lake Samra and Lake Lisan. The sedimentary history of these lakes was recon-structed by means of 230Th/234U ages of 30 samples, mostly of argonite laminae, from 8 columnar sections up to 110 km apart. The general validity of the ages was demonstrated by subjecting them to tests of internal isotopic consistency, agreement with stratigraphic order, and concordance with 14C ages. In the south, only the part of the Samra Formation older than 170,000 yr is exposed, while the aragonite-detritus rhythmites found in the central and northern region are generally younger than 120,000 yr. The Lisan Formation started accumulating about 63,000 yr B.P., with the clay and aragonite beds in the south-central area reflecting a rise in water level to at least −280 m. The upper part of the Lisan Formation, the aragonite-rich White Cliff Member, started accumulating about 36,000 yr B.P. The lake probably reached its highest level sometime after this, based on the ages of Lisan sediments preserved in the southernmost reaches of the basin.


2016 ◽  
Vol 5 (2) ◽  
pp. 244
Author(s):  
Uri Kafri

<p class="emsd-body"><span lang="EN-GB">A deep core hole, drilled in the middle of the Dead Sea penetrated the Pleistocene- Holocene section, revealed an alternating sequence of fresh water and evaporitic (gypsum, halite) deposits. The vertical facies variations were interpreted as related mainly to lake level changes during this period. The present study, however, proposes an additional factor that influenced these changes, namely subsurface seawater intrusion from the Mediterranean Sea to the endorheic Dead Sea Basin. This proposed process is controlled by the elevation and head difference between both base levels at a given time, because the Mediterranean Sea level also fluctuated during the discussed period. We find that in times of smaller head differences, and assumed lower seawater intrusion, a gypsum facies prevailed in the Dead Sea Basin. In times of greater head differences and assumed more abundant seawater intrusion a halite facies prevailed because of greater sodium chloride input into the Dead Sea.</span></p>


2006 ◽  
Vol 55 (3) ◽  
pp. 129-139 ◽  
Author(s):  
Avihu Ginzburg ◽  
Moshe Reshef ◽  
Zvi Ben-Avraham ◽  
Uri Schattner

2004 ◽  
Vol 141 (5) ◽  
pp. 565-572 ◽  
Author(s):  
YUVAL BARTOV ◽  
AMIR SAGY

A newly discovered active small-scale pull-apart (Mor structure), located in the western part of the Dead Sea Basin, shows recent basin-parallel extension and strike-slip faulting, and offers a rare view of pull-apart internal structure. The Mor structure is bounded by N–S-trending strike-slip faults, and cross-cut by low-angle, E–W-trending normal faults. The geometry of this pull-apart suggests that displacement between the two stepped N–S strike-slip faults of the Mor structure is transferred by the extension associated with the normal faults. The continuing deformation in this structure is evident by the observation of at least three deformation episodes between 50 ka and present. The calculated sinistral slip-rate is 3.5 mm/yr over the last 30 000 years. This slip rate indicates that the Mor structure overlies the currently most active strike-slip fault within the western border of the Dead Sea pull-apart. The Mor structure is an example of a small pull-apart basin developed within a larger pull-apart. This type of hierarchy in pull-apart structures is an indication for their ongoing evolution.


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