A day of geological exploration in the Negev: the En Yorqeam Formation (Upper Cretaceous) at Makhtesh Ramon

12_EnYorqeamView070813MITZPE RAMON, ISRAEL–Our final stop on our geological tour today was close to our temporary home: on the northern rim of Makhtesh Ramon (N 30.62831°, E 34.81759). Exposed here is the En Yorqeam Formation (Upper Cretaceous, Cenomanian), seen above as the less resistant marly unit between two resistant limestones. I did my first presentation on Israeli geology with bored and encrusted oysters from the En Yorqeam, which were also the subjects of a Fossil of the Week post.

We visited this outcrop today because there are some stratigraphic questions about its thickness and distribution. Its rich fossil fauna has also not been described in detail. This would be an ideal Independent Study project someday, especially with one large outcrop so close to our headquarters.

13_Echinoids070813Echinoids are the stars of the fossil fauna in the En Yorqeam. In just ten minutes we picked up over a dozen well preserved specimens. The large ones at the top are Heterodiadema lybicum. I don’t know the identity of the two in the bottom row. I bet some sharp student, though, can come up with the names quickly!

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A day of geological exploration in the Negev: Matred Formation fossils and bonus petroglyphs

8_OscarSilicifiedRingMatred070813MITZPE RAMON, ISRAEL–Our third stop in our geological journey today was 19 km north of Mitzpe Ramon (N 30.76084°, E 34.72020°) at another outcrop of the Matred Formation (Middle Eocene). We again had silicification, but no corals this time, The silica replaced the original limestone in a very strange way, producing these dark rings. Since silica is harder than limestone, the surrounding unreplaced limestone erodes faster, leaving the silicified rings in relief. They look anthropogenic, but they’re entirely natural. Again, mysteries abound.

9_SilicifiedBivalvesMatred070813In this close view of the silicified limestone are numerous bivalve shells that were replaced with silica just like the matrix. They appear to be a random distribution of shells with no preferred orientation.

10_SilicifiedFossil070813There are two fossils here replaced with silica. We’ll let the readers guess what they are.

11_Petroglyph070813These curious rings of black rock on the top of a hill attracted local peoples. Over the centuries (no one knows exactly how many or when) they carved numerous petroglyphs through the patina on the rock surfaces. We will also entertain guesses as to what is represented here!

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A day of geological exploration in the Negev: Silicified corals in the Matred Formation (Eocene)

MatredFormationView070813MITZPE RAMON, ISRAEL–Our next stop on this day of exploration was 32 km southeast of Mitzpe Ramon at outcrops of the Matred Formation (Middle Eocene). The location is N 30.36899°, E 34.98655°. Look at those coordinates on Google Maps and you’ll see that they are from the peak of that black mountain on the right of the above view. The black color is from the weathering of thoroughly-silicified (infused with silica) coral-rich limestones. Ordinarily paleontologists tend to stay away from such preservation because the matrix as well as the fossils are coarse, hard chert. These fossils, though, are important because they give strong clues about the depositional environment of the sediments. In this case, in situ coral reefs mean shallow water.

MatredCoral070813This is what the silicified corals look like in this part of the Matred Formation. We are looking down on the top of a colony. The holes represent the original corallites. Material like this cannot be identified to more than the family or genus, but we see enough to know that they are corals.

NummulitesMatred070813In this piece the bean-shaped fossils are large benthic foraminiferans that still retain their original calcareous skeletons. The matrix around them has been silicified. This type of preservation remains a mystery, especially when in the same unit we see the same fossils have been silicified and the matrix is not. More geological puzzles!

WadiView070813This wadi near the site is so beautiful I wanted to include an image. This would be a fun place to work, although maybe the spring would be more hospitable!

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A day of geological exploration in the Negev: the Hazeva Formation (Lower Miocene)

1_NachalParanFault070813MITZPE RAMON, ISRAEL–It is a tradition with the Wooster Israel expeditions to spend one day with our colleague Yoav Avni geologically explore areas beyond those associated with our present research topics. This is the way we plant seeds for future research endeavors — and Senior Independent Study projects. Today we went to four sites, which I will present in brief vignettes.

Our first stop of the day was in Nachal Paran at N 30.32329°, E 34.96388° about 35 km southeast of Mitzpe Ramon. The image of above is from our outcrop looking up at the faulted boundary of a large graben in which the valley is formed. Preserved within this down-dropped structure is a thick section of the Lower Miocene Hazeva Formation.

2_HazevaFormation070813Most of the Hazeva consists of reddish sandstones and conglomerates deposited by a very large river system that was flowing from the Arabian Peninsula into the Mediterranean. There have been a variety of African-derived mammal fossils in this unit, including elephants and giraffes. The unit of interest for us today is the gray rock at the base of the above image. It is a thin limestone unit no more than one meter thick. Its top has a scalloped pattern that may be due to ancient karstic weathering when the river deposited muds and gravels upon it. It appears to be a lake deposit formed just before the river moved into the region.

3_HazevaCloser070813Team Israel 2013 is here looking at a cross-section of the lacustrine (lake-formed) limestone and the sediments beneath it. One of the issues is how do we know that the limestone was formed in a lake. The best clue is the occurrence of tiny high-spired gastropods throughout the matrix. Another would be the presence of trace fossils that may represent the horizontal trails of snails and/or freshwater arthropods like isopods or insects. There is a pervasive pattern of vertical tubes that remains mysterious. Are they trace fossils or some sort of diagenetic phenomenon? A further question is why this lake was there in the first place considering that it sits in a section almost entirely formed of typical terrestrial siliciclastic sediments. Does it represent a brief climate change? A tectonically-induced change in the local hydrogeology? Plenty of questions here for future geological researchers.

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Goodbye, Makhtesh Gadol (for now)

GoodbyeMakhteshGadol070713MITZPE RAMON, ISRAEL–Today Team Israel 2013 had its last visit to Makhtesh Gadol, marking the end of Lizzie Reinthal’s and Steph Bosch’s fieldwork. We collected our last specimens from the Matmor Formation, which is exposed only in the center of this magnificent structure. The students above are looking down into the northern part of the makhtesh from the viewpoint at Mount Avnon.

MakhteshGadol070713This is a view from the same spot looking south along the western wall of the makhtesh. You can see a bit of the curvy, narrow road below that we used to enter and exit the makhtesh. This road was built by the British during World War II when they thought there might be oil underneath this breached anticline.

MG_BronzeAgeStructure070713This ring of stones is the remnant of a Bronze Age livestock pen, along with a probable small shelter for the shepherd in the lower left. This features are found throughout Makhtesh Gadol, usually up on the flanks of the walls or the Matmor Hills. I happened to come across this one in today’s walkabout.

LastCollecting070713Finally, here are students collecting at our last site — the southernmost exposure of the echinoderm-rich subunit we’ve found to be so productive. This morning we found … wait for it … two more bryozoans! This is usually not big news in most of the places I’ve worked, but it sure is here. They are again runner-types, but not Stomatopora. Much more to report on these after we get back home with them.

We still have five more working days in Israel. One will be devoted to finishing Oscar’s fieldwork, one to finishing smaller projects in the Makhtesh Ramon area, one to exploration of geological sites Yoav has chosen for us, one for a trip to Jerusalem and the headquarters of the Geological Survey of Israel, and a final day to make sure we’ve done all we came to do.

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Wooster’s Fossil of the Week: An echinoid from the Eocene of France

585 Echinolampas ovalis M Eocene Civrac-en-Médoc FranceThe above is a specimen of the echinoid Echinolampas ovalis (Bory de St Vincent, 1824) from the Eocene of Civrac-en-Médoc, France. We are looking at what is called the aboral surface — that part of the organism on the other side of its mouth. (I’m sure by now you recognize the little barnacle boring near the bottom of the skeleton.) Below is the oral view of the same specimen.585 Echinolampas ovalis M Eocene Civrac-en-Médoc France oral

Echinoids are a kind of echinoderm with a very long evolutionary history from the Ordovician to today. They include sea urchins, heart urchins and sad dollars, along with a few others. All echinoids are covered in life with numerous spines. These spines almost always fall off after the death of the organism, leaving the smooth test we see here. The tiny circles covering the surfaces of this specimen are spine attachments. In life this would have looked like a spiky ball.

In the center of the oral view is a large hole where the mouth was. The plates surrounding this are called the peristome (around-mouth). At the bottom on the oral view are two holes. The larger is where the anus was located (within the periproct of plates); the smaller is a circular boring, likely from a gastropod predator. Since the periproct is not in the center of the aboral surface, this is what is known as an irregular echinoid.
Echinolampas_ovalis_Eocene_Civrac-en-Médoc_France_CloseUp052013Above is a close-up of the center of the aboral surface. The radiating rows of holes were where tubefeet extended. These soft structures at the end of the water vascular system were used for locomotion, moving bits of food towards the mouth, and even respiration. The very center is a finely-porous plate called the madreporite (the opening for the water vascular system). The four holes around it are genital pores for releasing gametes into the water during reproduction. For a simple, globular organism, the echinoid is amazingly complex.
450px-Bory_Saint-Vincent_1778-1846Echinolampas ovalis was named by a scientist with a complex life story of his own. The dashing Jean Baptiste Bory de Saint-Vincent (1778-1846) was one of a remarkable generation of French zoologists. He began his career as a naturalist, studying the fauna on various French possessions in the Indian Ocean. He returned to France and became a soldier in the Napoleonic Wars, serving in the battles of Ulm (1805) and Austerlitz (1805), and participating in the disastrous French campaign in Spain. He was a Bonapartist to the end, opposing the Bourbon restoration, which resulted in exile from France. After his politics faded, he returned to France in 1820 and resumed his career as a traveling naturalist. He named dozens of living and fossil species of invertebrates after the wars, including our quiet little echinoid in 1824.

References:

Kier, P.M. 1962. Revision of the cassiduloid echinoids. Smithsonian Miscellaneous Collections 144(3), 262 pp.

Roman, J. 1965. Morphologie et evolution des Echinolampas (Echinides, Cassiduloides). Memoires du Museum National d’Histoire Naturelle, Nouvelle Serie, C, 15, 1-341.

Thum, A.B. and Allen, J.C. 1976. Reproductive ecology of the lamp urchin Echinolampas crassa (Bell), 1880 from a subtidal biogenous ripple train. Transactions of the Royal Society of South Africa 42: 23-33.

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Geoarchaeology in Timna Valley

StephChalcolithicMine070613MITZPE RAMON, ISRAEL–Wooster senior Steph Bosch is a double major in archaeology and geology. Rather than do a joint Independent Study project, she is actually doing two theses, which will no doubt be challenging this coming academic year, but she is more than a match for the task. Because of her interest in ancient mining, after our trip to Eilat we stopped by Timna Valley to look at some of the oldest mines in the world. Here she is inside a Chalcolithic copper mine at least 6000 years old. It was carved into the relatively soft Cambrian sandstone with stone tools, the marks of some of which can still be seen on the walls. (Elyssa Belding Krivicich will remember sitting in that same place for a photograph back in the day!) I am amazed we could crawl through a warren of these ancient mines, but then the surrounding mountains are riddled with hundreds that are well protected.

TimnaMushroom070613The landscape is fascinating, especially for geologists. The Cambrian sandstone is colorful and easily eroded, producing hoodoos like these as remnants on an intrusive igneous rock substrate.

TimnaArches070613That soft sandstone also weathers into natural arches, two of which you should be able to find in this view of the western wall of the valley.

TimnaSmeltingCamp070613During the 14th through the 12th centuries BCE, the Egyptians had an elaborate and extensive mining and production system at Timna. Here are the remains of a smelting camp where ore was processed to make ingots of copper. In this area is the smelter, a shrine, and a work building that had several rooms, each for a particular industrial purpose.

TimnaSmelter070613The smelter is easy to find because it is still to this day surrounded by fragments of black, glassy slag, a byproduct of the process.

OreCopperTimna070613The copper ore itself is easily seen as green-blue veins in the nearly white sandstone. The sandstone is very porous (it apparently represents the cross-bedded deposits of ancient braided streams) and is easily penetrated by hot waters generated by magmatic activity below. It appears to me to be the copper silicate mineral Chrysocolla.

Timna was a great place to look at the intersection of geology and archaeology.

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Wooster Geologists at the Red Sea

OscarStephLizzieRedSea070613MITZPE RAMON, ISRAEL–It is a tradition for Wooster Geologists in Israel to have a day trip on Saturdays (Shabbat) to places of geological and paleontological interest. This year we choose to go two hours south to the city of Eilat on the tiny Israeli coast of the Red Sea. We visited the Underwater Observatory Marine Park with its observation tower that extends above the sea for a view of the coastlines of four countries (Egypt, Israel, Jordan and Saudi Arabia) and below sea level for a glass-enclosed experience with the fish and corals. It was plenty warm, and the humidity was a bit of a shock after a week in the desert, but the breezes were very pleasant. Above is, from the left, Oscar Mmari, Steph Bosch and Lizzie Reinthal.

EilatCoastline070613This is the coastline to the east of the observatory looking into Eilat. You can see the fringing reef in the shallow water. Unfortunately, as you may have guessed, most of the reef is dead or dying. Coral reefs are stressed all over the world with climate change (warming and acidification, especially) and pollution, but those in the Red Sea are in particular trouble. This is a narrow, busy seaway so pollutants are not easily flushed out of the ecosystem. For more on this topic, see the post from a visit in 2011.

StephLizzieCoral070613Steph and Lizzie, framed by the marine invertebrates we all love so much.

Our visit was much fun as we got to see many denizens of the Red Sea, including turtles, stingrays, sharks, octopuses, crustaceans, and many diverse reef fish. It was also educational as we could see many recent analogues for our ancient fossil communities.

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Bryozoans finally make an appearance in the Jurassic of southern Israel

MatmorCollecting070513MITZPE RAMON, ISRAEL–The concentrated effort of all four Wooster Geologists in Israel finally paid off in fossil bryozoans today. Steph Bosch (center) is studying the bryozoans of the Matmor Formation (Middle Jurassic) in Makhtesh Gadol for her Independent Study project. We have bryozoan specimens collected on earlier expeditions to the Matmor, but on this trip have been stymied in our efforts to add to the meager collection. Bryozoans are rare in these equatorial sediments, even though the diversity of other fossils here is very high. We want to describe this fauna for the first time and place it in its environmental and evolutionary context.

This afternoon we visited a site at the far northeastern end of the makhtesh where we knew lots of crinoids were preserved. (The locality is creatively known as “GPS 004”; N 30.94916°, E 35.01110°.) Our working hypothesis is that bryozoans preferred the same conditions as echinoderms in the Matmor Sea. The strategy worked: we found two runner-type bryozoans on crinoid columns. They are the stomatoporid-type of uniserial runner, giving us at least two different species of bryozoan now from the Matmor. Undoubtedly there are more such specimens on the many crinoid ossicles we collected to wash and examine later in the Wooster lab. They are far too small to photograph here in my hotel room!

Steph, appropriately, found the first specimen. Oscar Mmari (on the left) found the second just as we were leaving. Lizzie Reinthal (on the right) is actually working on crinoid taphonomy, so she was very pleased by all the specimens we collected today.

MatmorCollectingView070513A wider view of our collecting site in the Matmor Formation, with the northeastern wall of Makhtesh Gadol in the background.

It feels good to now have all three Wooster seniors with materials they’ve collected for their Independent Study projects. A nice way to end our first week of work in Israel!

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An outcrop Dr. Judge would love (Upper Cretaceous of southern Israel)

WadiHavarimDragFold070513MITZPE RAMON, ISRAEL–Wooster Geologists Oscar Mmari’s Independent Study project on the Late Cretaceous phosphorites in the Negev has become multidimensional. His most interesting section is in Wadi Hawarim, where we returned today with Yoav Avni for additional observations and measurements. We are now doing a bit of structural geology that Dr. Shelley Judge would appreciate. In this view above, the dark resistant unit on the left is the lower silicified portion of the Mishash Formation (Upper Cretaceous). Even though it looks like an igneous intrusion, these are sedimentary beds folded so that they are vertical in attitude. On the right you may be able to make out Oscar standing on Mishash beds that are almost horizontal. How does this make sense?

What happened was faulting on the farthest left in this view above. A normal fault perpendicular to this screen has its upthrown block on the left and downthrown block on the right (where Oscar is standing). The Mishash silicified rocks are part of a drag fold as the blocks moved against each other. It appears that this faulting took place while the rest of the Mishash was still accumulating because debris from the silicified layers was spread over the phosphorites as they developed. There may also have been a shallowing of sealevel indicated by a layer colonized by shrimp who made Thalassinoides burrow systems that became inundated with siliciclastic sediment likely derived from the fault scarp.

OscarWadiHavarim070513In this view into Wadi Havarim, the whitish phosphorite beds of the Mishash Formation are in the center above a dark conglomerate and below the yellowish Ghareb Formation.

OscarAtWork070513Oscar is sitting on Mishash conglomerate taking careful notes on this complex geological scenario. He’s going to need his skills in structural geology, sedimentology, stratigraphy and paleontology for this project!

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