Stegodon: Does this ancient elephant have origins in Asia?

So much has been said in recent years about the wealth of fossils in China. Almost all of it about dinosaurs: exciting new species, feathered fossils, nest upon nest of dinosaur eggs.  There is no doubt that China holds exciting clues to the history of our planet; one has only to wait to hear of the next discovery.

Within the past few months, yet another exciting find was revealed, but this time about a little known mammalian ancestor: Stegodon.

 

Stegodon by artist Hannah Stephens

Painting of a Stegodon by artist Hannah Stephenshannahleestudio.com.

 

The name Stegodon, to me, evokes ‘dinosaur’, not ‘mammal,’ but this was, indeed, an ancient animal.  Its fossils resemble those of other similar mammals, from mastodons to mammoths to today’s elephants.

 

 

Alexandra van der Geer - shrinking elephants

Figure 1: Reconstruction of four insular dwarf proboscideans with their respective mainland ancestors. Mainland proboscideans: 1, Palaeoloxodon antiquus; 2, Mammuthus columbi; 3, Stegodon zdanskyi [stegodon found in China]. Insular proboscideans: 4, Palaeoloxodon ‘mnaidriensis’; 5, Palaeoloxodon falconeri; 6, Mammuthus exilis; 7, Stegodon aurorae [a type of dwarf stegodon found in Japan]. Based on skeletons at Museo di Paleontología, University of Rome, Italy (1), American Museum of Natural History, New York (2), Taylor Made Fossils, U.S. (3), Museo di Paleontología e Geología G.G. Gemmellaro, Palermo, Italy (4), Forschungsinstitut und Naturmuseum Senckenberg, Frankfurt, Germany (5), Santa Barbara Museum of Natural History, Santa Barbara, U.S. (6), Taga Town Museum, Honshu, Japan (7). Photos 1–2, 4–7 George Lyras, photo 3 courtesy of TaylorMadeFossils.com, reproduced here with permission.

From The effect of area and isolation on insular dwarf proboscidea by Alexandra A. E. van der Geer et al; photo and caption courtesy of Dr. Alexandra van der Geer.

 

When Stegodon skulls with tusks attached have been found, many (but not all) of the tusks are close together–preventing the trunk (the ‘proboscis,’ from which this group gets its name; proboscis —> proboscidea) from hanging between them.

They lived in what is now Africa and Asia, causing continued debate over its place of origin. Until recently, the oldest known Stegodon fossil, a 6.5+ million-year-old partial molar from Kenya, was described by William J. Sanders in 1999.  That record changed this past December when Dr. Hong Ao and his colleagues published their results dating the sediment in the Lanzhou Basin, China, from which a number of fossils–including that of a Stegodon–were found.

And that Stegodon was found to be between 8 – 11 million years old.

 

GSA Geologic Time Scale - Neogene

Detail of the Geologic Time Scale, created by the Geological Society of America.  Stegodon is believed to have existed between the Miocene to the Pleistocene, a relatively small segment of time in Earth’s overall history, but still considerably longer than that of our own species!  (You can view the time scale in much better detail here.) 

 

The fossils of the Stegodon, along with at least 5 other species, were actually found in the 1980s by Professor Xing Zhang of Northwest University in China.  Given the length of time between the fossil excavations and the recent dating of these fossils, one might wonder why determining the fossil age took so long.

Dr. Ao, a scientist at the State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, and his colleagues state that western China does not have suitable material for radiometric dating, an oft-used method for this purpose.

When I asked why this was so, Dr. Ao replied by email, “Because volcanic activities are rare in western China during the late Cenozoic, it is difficult to find  in situ tephros or tuffs for radiometric dating (e.g., 40Ar/39Ar dating).”

Instead, they conducted a magnetostratigraphic study, one in which they determined the age of the rock through the polar reversal record.  Combining this with analysis of the fossils provided evidence that this Stegodon is 2 – 5 million years older than that of the Kenyan partial molar.

“We are indeed surprised by our dating results,” Dr. Ao continued, “which document that the Lanzhou Stegodon is the oldest Stegodon worldwide, although the Stegodon  fossil [was] not discovered by us. However, our dating results document it to be the oldest known Stegodon fossil.”

Dr. Hong Ao 1

 

Dr. Hong Ao 2

Dr. Hong Ao 3

Dr. Hong Ao 4

Images of Professor Yongxiang Li (from Northwest University) and his master student as well as several employed workers who helped to excavate mammal fossils, Lanzhou Basin, China; photos courtesy of Dr. Hong Ao.

 

indricotherine fossil

indricotherine fossil2

indricotherine fossil3

Images of indricotherine fossils found in Lanzhou Basin, China; photos courtesy of Dr. Hong Ao.

 

Dr. Ao himself has been working with fossils in the Lanzhou Basin for 5 years.  When asked how  he and his co-authors chose to work together on this recent paper, he wrote, “I have collaborated with them on broad subjects before, thus I [invited] them to join [in] this research.”

Finding information about this extinct species is difficult.  Unlike mammoths or mastodons, Stegodon does not appear to be a popular ancient animal.

Fortunately, Dr. Alexandra van der Geer–paleontologist, indologist, ethno-zoologist and author –has not only studied this species, she very generously made herself available for questions.  Currently, Dr. van der Geer is an Associate Researcher at both the National and Kapodistrian University of Athens and the Naturalis Biodiversity Center in the Netherlands. She is part of the Isolario project, a project that studies biodiversity and cultural evolution within an island context.

When I asked why there was such a dearth of information on Stegodon, she wrote, “We can think of several reasons for this.”

“First of all, stegodons typically are the elephants of Southeast and East Asia, where most countries did not have the resources and opportunities most Western countries had when it comes to scientific research and excavations. These activities are costly, and since they don’t have a direct use in the sense that they don’t advance the medical, technical or economic levels of a country, they have, understandably, a lower priority. Furthermore, because of this region, half the publications (especially before the 1990s or so) you can find are in Chinese or Japanese, which is not very helpful to the [English-speaking] world.

“Secondly, stegodons are forest elephants. Forest areas are very unlikely places for the long-term preservation of organic materials: everything is eaten, digested or otherwise broken down into smaller components in no time. The tropical (warm, humid) climate of these forests is not helpful either, as decomposition is much faster here. Stegodon remains only have a chance to be preserved when (1) they are covered fast, such as with river sediments, volcanic ashes etc., (2) or are in an oxygen-free environment, such as sunken deeply into a swamp, (3) or were deposited in a natural fridge such as limestone caves where they are gradually covered in clayish sediment or [travertines]. The same is valid for Palaeoloxodon, the Old World fossil elephant, but Europe has many limestone caves, which are excellent for preservation (for a nice [travertine]-preserved negative skull, see Stuttgart museum: skull cast SMNS nr. 32888 from Bad Cannstatt).

“As you can deduct from these preservation issues, it is more likely to find molars and tusks than skeletal material, which is much softer. The vast majority of proboscidean findings all over the planet consists of molars and tusks, and that is not for nothing. Inherently this means that there is much more information about their dentition and diet than about their bodies.”

I was interested in understanding why Stegodons are portrayed as hairless animals, so very similar to contemporary elephants.  Was this just an artistic guess?

“The hairlessness of stegodons is not an artistic guess but a scientific guess instead,” Dr. van der Geer answered.  “Very large animals with thick skins (pachyderms) in a (sub)tropical environment are unlikely to have a significant hair covering. Elephants lost their hairs secondarily. The information for hair growth is not lost, and baby elephants still have a thin, woolly coat. Woolly mammoths lived in the cold, temperate zones, and needed hair, so they were covered in a thick layer of hairs, and for this is evidence (mummies preserved in the permafrost), but the other mammoths (M. meridionalis, M. columbi, M. exilis, etc.), [did] not, and it’s generally assumed that they had a light coat fitting to the temperate zones.

“Tropical and subtropical stegodons almost certainly did not have any coat that’s worth mentioning. Stegodons of temperate zones, however, may have been more hairy. Indeed, the lack of hairs makes them look more like today’s elephants.”

 

Alexandra van der Geer - Stegodon ganesa-model-I.Vjdchauhan-SiwalikHills

Photo of the two life-size models of Stegodon ganesa;photo courtesy of Dr. Gerrit van den Bergh (University of Woolongong, Australia); special thanks to Dr. Alexandra van der Geer.

 

“Note, however, that the proboscis is carried very differently. Their tusks are set very close to each other, so the proboscis doesn’t fit in between as in modern elephants, Asian and African alike. This means that the mobility of their proboscis was more restricted, relative to their living relatives.”

 

Alexandra van der Geer - Flores-excavation-31-stegodon-florensis

Fossils of Stegodon florensis insularis, from Flores, Indonesia; photo courtesy of Dr. John de Vos (Naturalis, the Netherlands); special thanks to Dr. Alexandra van der Geer.

 

Alexandra van der Geer - stegodon-timorensis-mandible

Mandible (and holotype!) of  Stegodon timorensis; photo courtesy of Eelco Kruidenier (Naturalis, the Netherlands); special thanks to Dr. Alexandra van der Geer.  Anyone familiar with proboscidean teeth and jaws will recognize the similarities instantly.

 

But how do we know that Stegodon–a rather enormous animal–evolved into something smaller?

“[D]warfs and giants are relative. Something can be a dwarf, yet have a considerable size. When we speak of dwarf stegodons, we mean stegodons that are much smaller than their ancestors. For this, you have of course to have identical or otherwise similar elements from both the descendant and the ancestor in order to compare reliably,” she continued.

“The expectation is that dwarf stegodons must have existed on the islands, following the so-called island rule, according to which large animals get smaller in isolation. There is sound evidence that this rule still stands, and is even more pronounced for fossil species (see Lomolino et al., 2013, in Journal of Biogeography).

“Indeed, the many fossil molars from the Southeast Asian islands (‘Wallacea’) are all much and much smaller than the same molars from their mainland ancestors (see Van den Bergh, 1999). True, you first have to know what is the ancestor, and for this you need information about morphology, or how the molars, tusks, skulls and postcranial elements look like. After that, you compare the sizes.

“Note that if a molar is, for example, half the length of the same molar of its ancestral species, the body weight of that animal must have been a quarter of that of its ancestor! (the cubic law: linear reduction 50% means volume reduction 50% of 50%).”

Alexandra van der Geer - Flores-stegodon-florensis

Molar of Stegodon florensis; photo courtesy of Dr. Gerrit van den Bergh (University of Woolongong, Australia); special thanks to Dr. Alexandra van der Geer.  

 

“The most interesting dwarf stegodon is Stegodon sondaari, named after the Dutch palaeontologist Paul Yves Sondaar (1934-2003), expert in fossil insular mammals. This stegodon lived on the island of Flores about a million years ago, and weighted only about 15% of the weight of its ancestral species, S. elephantoides (see Van der Geer et al., 2016, in Journal of Biogeography, doi:10.1111/jbi.12743).

“Sondaar’s dwarf stegodon is not the smallest stegodon, that honour goes to the Sumba stegodon (S. sumbaensis), of only 8% of the original weight. Sondaar’s stegodon is interesting because it may have witnessed the arrival of early humans, possibly the ancestors of the Hobbit, or Homo floresiensis. Its fossils are contemporaneous with primitive lithic artefacts, dated to about a million years ago (see Brumm et al., 2010, in Nature 464, pp. 748–752).”

 

Alexandra van der Geer - Sumba-stegodon-sompoensis-holotype-in-Naturalis-Leiden-2

Molar (and holotype!) of Stegodon sompoenisphoto courtesy of Dr. Gerrit van den Bergh (University of Woolongong, Australia); special thanks to Dr. Alexandra van der Geer.  

 

“[R]ecently,” she concluded, “one of the island dwarf stegodons (S. timorensis of Timor) has been dated to about 130 thousand years ago (see Louys et al., 2016, in PeerJ 4:e1788). This excludes, according to the authors, an anthropogenic cause for its extinction, because humans had not yet arrived at the island.”

 

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So many people helped with this blog post!  (But please remember that any errors are my own.)

Many, many thanks to Dr. Hong Ao (Dr. Ao Hong) from the State Key Laboratory of Loess and Quaternary Geology (Chinese Academy of Sciences) for his fascinating responses and the great images of fossil excavations in the Lanzhou Basin.  I am thrilled that he was willing to answer questions about his research and that of his colleagues! It was a great honor and a pleasure connecting with him!

I am indebted to Dr. Alexandra Van der Geer, who very kindly (and so very quickly–despite everything else she has going on!!) answered specific questions about Stegodon that I could not find anywhere else and who provided pictures of dwarf Stegodon fossils.  It was an equally great honor and pleasure connecting with her!

A mastodon-sized thank you to the amazing Dr. Katy Smith for providing needed and hard-to-find material on Stegodon fossils!

And an enormous thank you to artist Hannah Stephens for her depiction of a Stegodon as it may have appeared in life.  I am particularly moved by the warmth of its intelligent-looking eyes, and I love the tones within its skin.  I adore this picture.  I am grateful to have it in this post;  I am thrilled to have the actual painting hanging on my wall!  Please be sure to check out her artwork at: http://hannahleestudio.com or http://hstephens.blogspot.com

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References from Dr. Alexandra Van der Geer:

  1. Brumm A, Jensen GM, van den Bergh GD, Morwood MJ, Kurniawan I, Aziz F, Storey M (2010) Hominins on Flores, Indonesia, by one million years ago. Nature 464, 748–752.
  2. Lomolino MV, van der Geer AAE, Lyras GA, Palombo MR, Sax DF, Rozzi R (2013) Of mice and mammoths: generality and antiquity of the island rule. Journal of Biogeography 40, 1427–1439.
  3. Louys J, Price GJ, O’Connor S. (2016) Direct dating of Pleistocene stegodon from Timor Island, East Nusa Tenggara. PeerJ 4:e1788
  4. van den Bergh GD (1999) The Late Neogene elephantoidbearing faunas of Indonesia and their palaeozoogeographic implications; a study of the terrestrial faunal succession of Sulawesi, Flores and Java, including evidence for early hominid dispersal east of Wallace’s line. Scripta Geologica 117, 1–419.
  5. van der Geer AAE, van den Bergh GD, Lyras GA, Prasetyo UW, Due RA, Setiyabudi E, Drinia H (2016) The effect of area and isolation on insular dwarf proboscideans. Journal of Biogeography, doi: 10.111/jbi.12743

References used in this blog post:

  1. New magnetochronology of Late Miocene mammal fauna, NE Tibetan Plateau, China: Mammal migration and paleoenvironments; by Hong Ao, Peng Zhang, Mark J. Dekkers, Andrew P. Roberts, Zhisheng An, Yongxiang Li, Fengyan Lu, Shan Lin, Xingwen Li; Earth and Planetary Science Letters; 1o December 2015
  2. Oldest record of Stegodon (Mammalia: Proboscidea); by William J. Sanders; Journal of Vertebrate Paleontology; Vol. 19, No. 4, Dec. 13, 1999, pp. 793 – 797
  3. Fossil elephantoids, Awash paleolake basins, and the Afar triple junction, Ethiopia; by Jon E. Kalb; Palaeogeography, Palaeoclimatology, Palaeoecology; 1995, pp. 357 – 368
  4. The effect of area and isolation on insular dwarf proboscidea; by Alexandra A. E. van der Geer, Gerrit D. van den Bergh, George A. Lyras, Unggul W. Prasetyo, Rokus Awe Due, Erick Setiyabudi, and Hara Drinia; Journal of Biogeography; 11 March 2016.
  5. Magnetostratigraphy – concepts, definitions, and applications, by Cor G. Langereis, Wout Krijgsman, Giovanni Muttoni, and Manfred Menning; Newsletter on Stratigraphy, Vol. 43/3: 207–233, April 2010
  6. Mammoths and Mastodons of the Ice Age, by Adrian Lister, Firefly Books, 2014
  7. Mammoths, by Adrian Lister and Paul Bahn, University of California Press, 2007
  8. The Proboscidea: Evolution and Palaeoecology of Elephants and Their Relatives, Edited by Jeheskiel Shoshani and Pascal Tassy, Oxford Science Publications, 1996
  • Stegodontidae: evolutionary relationships by Haruo Saegusa, pp. 178 – 190, The Proboscidea: Evolution and Palaeoecology of Elephants and Their Relatives
  • Palaeobiogeography of late Neogene African and Eurasian Elephantoidea by Jon E. Kalb, David J. Froehlich, and Gordon L. Bell, pp. 117 – 123, The Proboscidea: Evolution and Palaeoecology of Elephants and Their Relatives
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VI International Conference on Mammoths and Their Relatives – May 2014!

Every three to four years, mammoth experts and scientists from all over the world congregate for several days to discuss the most recent findings and cutting-edge discoveries.

This year, that event takes place in Greece.

This location is particularly fitting, not only for its exciting mammoth and mastodon finds (including the world’s largest tusks found to-date), but also because the name of the mammalian Order to which mammoths belong is derived from a Greek word: proboskis (προβοσκίδα).

The name Proboscidea–from proboscis (trunk)—aptly describes some of its more popular members: today’s elephants and yesterday’s mastodons and mammoths.

This marks the 6th time this conference has been held.  It is not an annual event, nor is it necessarily held in the same location or on the same continent.

This year’s honorary president is a US-based scientist: Dr. Larry Agenbroad, from the Mammoth Site in Hot Springs, South Dakota.

Dr. Larry Agenbroad

(Image of Dr. Larry Agenbroad with short-faced bear replica, courtesy of Dr. Larry Agenbroad)

The president of the conference is Dr. Evangelia Tsoukala, Associate Professor of Geology at the University of Thessaloniki, and one of the team of paleontologists who excavated the largest tusks mentioned above.

The vice president is Dr. George Theodorou, Professor of Palaeontology and Stratigraphy at the National and Kapodistrian University of Athens.

The list of scientists and experts involved in this event is both impressive and exciting.  Among so many others, (there were too many to mention here, but you can find them at this link) some of the participating specialists are:

  • Dr. Paul Bahn, British archaeologist and co-author of Mammoths: Giants of the Ice Age with Dr. Adrian Lister;
  • Dr. Daniel Fisher, Professor at the University of Michigan, Curator and Director at the Museum of Paleontology, Michigan, mammoth-tusk expert, and one of the original scientists to study Lyuba, the best preserved baby mammoth found to-date;
  • Dr. Victoria Herridge of the Natural History Museum, London and dwarf mammoth expert;
  • Dr. Frédéric Lacombat, paleontologist at the Musée Crozatier, France, and president of the Vth International Mammoth Conference, 2010;
  • Dr. Adrian Lister of the Natural History Museum, London and author of the two most comprehensive books on mammoths published in English;
  • Dick Mol, mammoth expert from the Netherlands who has been involved in mammoth research and discoveries for decades, and one of the paleontologists who excavated the tusks in Greece with Dr. Tsoukala;
  • Dr. Doris Nagel of the Institute of Palaeontology, University of Vienna;
  • Dr. Maria Rita Palombo of the Università degli Studi di Roma La Sapienza;
  • Dr. Alexei Tikhonov, Deputy Director of the Zoological Institute, St. Petersburg,  Scientific Secretary of the Mammoth Committee, Russian Academy of Sciences, and also one of the scientists who originally studied Lyuba;
  • Dr. Haowen Tong, Adjunct Professor of the Graduate University, Chinese Academy of Sciences.

Historical Paleontological Collection of Siatista

(Image of the Historical Paleontological Collection of Siatista, Municipality of Voion, courtesy of the OC of the VIth ICMR)

Evangelos Vlachos, a PhD student at the Aristotle University of Thessaloniki and one of the many organizers of the event very generously responded to my questions.

———————————————

1. What will your PhD be in and what is your doctoral thesis? How did you become involved in the Mammoth Conference?

I am doing my PhD on Vertebrate Paleontology, specifically on the study of turtles and tortoises from Greece.

But what is a “turtle guy” doing at the Mammoth Conference?

Well, being part of Evangelia Tsoukala’s team includes excavating for proboscideans, including some of the biggest ever lived. In my first years of study, I considered working with fossil proboscideans, but later I changed to the study of chelonians.

My first experience with the Mammoth Conference was at the Vth Mammoth Conference in Le Puy-en-Velay, France in 2010.  In Le Puy, the Greek side participated with many oral and poster presentations, and the scientific community had the chance to get familiar with the exciting proboscidean findings from Greece.

Poster presentations of the Greek-Dutch team

[Image of poster presentations of the Greek-Dutch team during the Vth ICMR in Le-Puy-en-Velay, France (2010, picture credits W. van Logchem), courtesy of the OC of the VIth ICMR)]

2. How wonderful that the Mammoth Conference is held in Greece this year! How was the decision to hold it in Greece made?

Indeed, it is wonderful, but it was sudden!

Normally, at the end of each conference, the Organizing Committee examines all of the available proposals and decides where the next Mammoth Conference will be held.

In Le Puy, the Organizing Committee decided that Anchorage, Alaska would host the VIth Mammoth Conference in May 2013. Although the scientific community was excited to visit this remote place, which has played an important role in the history of the mammoths, things didn’t work out.

In the beginning of 2014, new proposals were requested. Within a few days, we filed a proposal to host the next conference in the historic towns of West Macedonia, Grevena and Siatista, which have brilliant collections of fossil proboscideans.

Luckily, our proposal was accepted, and we are honored to host the next conference in Greece.

Dutch artist Remie Bakker

[Children making their own mammoth under the guidance of the Dutch artist Remie Bakker, during the opening ceremony of the Historical Paleontological Collection of Siatista. Similar events are going to be held during the conference (2011, picture credits V. Makridis), image courtesy of the OC of the VIth ICMR)]

3. Who organizes this conference and who determines the president of the conference? (Do the organizers change each year?)

The organization of the conference is the responsibility of the Organizing Committee.

Some members are regular; they have been there since 1995 when the first conference was held in Saint Petersburg.

Specialists like Dick Mol provide the experience of organizing a Mammoth Conference and access to the network of the proboscidean scientific community.

Many people from the host country itself are involved to make sure that everything will be organized in detail. The organizers of the conference are supported by the Scientific Committee: specialists of various topics related to the conference. Their role is to consult the committee in scientific matters and to serve as reviewers of the abstracts and papers submitted to the conference.

This year, we are privileged to have a large Scientific Committee of 43 specialists from all fields related to proboscidean study. Moreover, in this conference, many young scientists are included in the Scientific Committee, which is very important for us. One of the goals of this conference is to ensure that the study of proboscideans will not only have a glorious past, but a great future as well.

4. Who typically attends this conference? Do you have an idea of how many people will be attending this year?

The Mammoth Conference attracts the interest of scientists from many different fields, but all joined by the interest of promoting knowledge surrounding proboscidean evolution.

Among the numerous participants, you will find paleontologists presenting new findings that improve our knowledge of the fossil record; geneticists examining the DNA of present-day elephants and from the frozen carcasses of the woolly mammoths; scientists applying new techniques like stable isotope and dental microwear analysis on proboscidean molars; archaeologists investigating the interaction between humans and proboscideans.

This is not all. At each conference, something new comes up!

Early registration for the participants closed on 31th of January 2014.

The interest of the proboscidean community in the VIth ICMR was enormous and far exceeded the expectations of the Organizing Committee!

We received more than 150 registrations from all corners of the world: from Cape Town, South Africa in the South to Stockholm, Sweden in the North; from Wollongong, Australia in the Southeast to Edmonton, Canada in the Northwest; from Kusatsu, Japan in the East to Nevada in the West; from Rio de Janeiro, Brazil in South America to Yakutsk in Siberia. In total, all the participants will have to travel more than 11 times the circumference of Earth to come to Grevena and Siatista!

Mammoth Conference Global Participants

 (Geographic representation of this year’s Mammoth Conference participants, image courtesy of the OC of the VIth ICMR))

5. How does one decide what topics and papers will be discussed?

The Organizing Committee, in close co-operation with the Scientific Committee, set an initial number of topics to be discussed in the conference. They have to summarize the current open questions in the field.

Some of the topics, however, are “classical,” we could say, such as the information from soft tissues from the frozen carcasses, or the interaction between humans and mammoths.

At the same time, in every conference we are trying to promote the regional research by proposing topics that could stimulate researchers to come up with ideas. For example, in our conference, we are particularly interested in the “primitive” probiscidean proboscidean forms–before the appearance of mammoths–like the mastodons or gomphotheres.

Sometimes, the participants are able to propose new topics of interest. This was the case with our Brazilian colleagues, who suggested we have a session on extinct South American proboscideans that, until recently, have been relatively unknown.

6. What do you think is the most exciting part of the Mammoth Conference?

As a young scientist, the most exciting part is definitely to get to know all the well-known specialists in this field and exchange ideas with them.

Standing up in front of a well-qualified audience and presenting your ideas is a great challenge. But the experience you get is unique.

Presentations - Vth ICMR

[Presenting in front of the world’s leading experts (Vth ICMR in Le-Puy-en-Velay, France, 2010, picture credits V. Makridis), image courtesy of the OC of the VIth ICMR)]

 

In the end, when you are returning to your country, you feel overwhelmed by the information you have received. But as the days go by, ideas start to form and with the experience gained by attending an International Conference, you can make good progress on your studies.

Science is not only reading and writing, but communicating your ideas.

Preparing a plaster jacket for a partial femur of a mastodon

[Preparing a plaster jacket for a partial femur of a mastodon. Now this specimen is part of the Paleontological Exhibition of Milia (2012, picture credits W. van Logchem), image courtesy of the OC of the VIth ICMR)]

Moreover, it is always exciting to take part in the field trips of the Conference.

In our conference, not only we will visit all of the impressive sites in Northern Greece, like Grevena, Milia, Siatista and Ptolemaida, but we have planned a unique post-conference field trip. The participants will travel to the remote island of Tilos where the last European elephants lived, as dwarf forms, in the Charkadio Cave. To reach this island, we will go through Athens and the world famous site of Pikermi.

Excavating in site Milia-4 using rope techniques

 

[Excavating in site Milia-4 using rope techniques. One of the sites that the participants will visit during the Field Sessions of the conference (2010, picture credits W. van Logchem), image courtesy of the OC of the VIth ICMR)]

 

7. Are there any challenges to organizing or hosting the Mammoth Conference?

One word: logistics.

The amount of work needed to arrange everything–the registrations, the abstracts, transportation and accommodation, the field trips–is enormous. In those cases, especially when you have so many people from different countries and cultures, you need to pay attention to every detail to make sure that all will go according to plan.

But the Organizing Committee is working hard, night and day, to extend an example of traditional Greek hospitality to everyone involved!
8. Is there anything else that you would want people to know?

Latest News:

This week, members of the Organizing Committee visited the places where the conference will take place (Grevena, Milia, Siatista and Ptolemaida) and inspected all venues, exhibition and facilities. At the moment, everything is going according to plan and the Organizing Committee works day and night to make a wonderful conference for the participants.

 Paleontological Exhibition of Milia

(Image of the the Paleontological Exhibition of Milia, Municipality of Grevena, courtesy of the OC of the VIth ICMR)

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I would like to extend an Archelon ischyros-sized thank you to Evangelos Vlachos for his lightning quick responses to my emails, his generosity and his detailed answers! 

When he mentions that the Organizing Committee works night-and-day for this conference, he is not kidding. Some of our emails were exchanged at 3am his time!  

Σας ευχαριστούμε!

Thank you, as well, to Dr. Evangelia Tsoukala and to Dick Mol, who also generously shared their time for this post (behind the scenes)!

Please check out the VI International Conference website:  www.mammothconference.com

You can follow them on Twitter! @mammoths2014 / #mammoths2014

Videos on YouTube related to the Conference and excavating the world’s longest tusks from the mastodon in Greece!

a. http://www.youtube.com/watch?v=caDUsZHehyY&list=UUJJtPaGIosoQiSHtBSyQ7RA&feature=c4-overview

(The video above is multilingual.)

b. https://www.youtube.com/watch?v=yCMDHJSTYZE&list=LLIWT11-xMeFd4CEztS2eB9g

c. https://www.youtube.com/watch?v=WJPB4Vdy70A&list=LLIWT11-xMeFd4CEztS2eB9g

It has been my great honor to have connected previously with two of the many mammoth experts listed above:

Dr. Daniel Fisher:

https://mostlymammoths.wordpress.com/2013/09/10/mammoth-article-qa-dr-daniel-fisher-renowned-paleontologist/

Dr. Larry Agenbroad:

https://mostlymammoths.wordpress.com/2014/01/23/the-mammoth-site-and-dr-larry-agenbroad-renowned-paleontologist/