MARQ and its Thematic Galleries

EDUCATIONAL PANELS

The amount of material found on archaeological sites can be very large and varied.  Archaeologists cannot know everything about such diverse subjects as zoology, geology or chemistry. They need help from other specialists in order to find out as much information as possible. 

The main corridor of the museum is divided into three sections with text panels that explain the auxiliary sciences of archaeology. 

FIRST INTERACTIVE AREA

The “Environmental Sciences” are grouped together and provide information about the environment and climate in the past. 

  • Sedimentology: This is the study of soil and geological sediments that are deposited on archaeological sites. They provide valuable information about natural phenomena, for example, ancient climate.
  • Palynology: This is the study of pollen remains that are preserved in archaeological layers. They help to identify what vegetation existed when the area was occupied. A microscope, like the ones here, is needed to analyse the pollen.
  • Carpology: This is the study of the remains of preserved (normally carbonized) fruit and seeds. These remains can help us know, for example, what types of vegetables and fruit people ate in the past. 
  • Anthracology: This is the analysis of charcoal remains. It helps identify the types of wood that were being used by people and provides us with information on past vegetation. 
  • Malacology: This is the study of mollusks – marine and terrestrial (snails) shells that are found on archaeological sites. They provide us with information about past environments and climate. 
  • Zooarchaeology: This is the study of animal remains found on archaeological sites. It not only provides information on the fauna of a certain period, but also provides information about human activities (eg hunting, fishing, raising cattle) and diet. 
Los paneles didácticos en el MARQ
Bandejas temáticas en el MARQ
Bandeja de Carpologia

DENDROCHRONOLOGY

This is a scientific method based on the dating of growth rings of tree trunks. A new ring is formed each year, and the width of the ring depends on environmental conditions (temperature, rain, etc..). An old tree has many rings. The same species of tree growing in the same area will have similar width rings. If we have trees from different periods in the same region, we can create a continuous time sequence from the present to the past.  Therefore, if we find a large piece of wood that has its rings, we can compare this to the sequence and be able to date when the tree was cut down and then used.

In the following example, a piece of wood from a Roman site is being dated. Follow the sequence and see how this is done. This is not a real example as it has been deliberately exaggerated to show clearly how this dating method works. In real examples, many more samples of wood are needed to be able to create a long sequence of dates that go far back into the past.

Bandeja de Dendrocronología

SECOND INTERACTIVE AREA

This section has been divided into the “Dating Sciences” and the “Human Sciences.”

The “Dating Sciences” are associated with dating. There are a number of different techniques, but these are the ones most commonly used:  

  • Dendrochronology: This is the study of tree rings from wood found on archaeological sites. They can be compared to well-established tree ring sequences to determine the tree’s age and the period during which it was being used (see previous page). 
  • Radiocarbon (C-14) Dating: This is currently the most precise method of dating. It can only be used for organic materials (charcoal, bone, seeds, wood, textile, or shell). The C-14 molecule is present in all living things on the planet. When an organism dies, the C-14 begins to slowly decay and disappear at a constant rate. This can be measured enabling us to calculate the time that has passed since the death of the organism. The drawing will help you understand this process better. 

The “Human Sciences” contribute to our understanding of the physical, social and cultural aspects of human life. 

  • Physical Anthropology: This is the study of human bones, often found in cemeteries, to find out the age and sex of an individual.
  • Palaeopathology: This is the study of ancient diseases by analysing bones.  It can also be used to identify the cause of death. 

Consuelo roca de togores muñoz

Specialist in physical anthropology

SECOND INTERACTIVE AREA

This section has been divided into the “Dating Sciences” and the “Human Sciences.”

The “Dating Sciences” are associated with dating. There are a number of different techniques, but these are the ones most commonly used:  

  • Dendrochronology: This is the study of tree rings from wood found on archaeological sites. They can be compared to well-established tree ring sequences to determine the tree’s age and the period during which it was being used (see previous page). 
  • Radiocarbon (C-14) Dating: This is currently the most precise method of dating. It can only be used for organic materials (charcoal, bone, seeds, wood, textile, or shell). The C-14 molecule is present in all living things on the planet. When an organism dies, the C-14 begins to slowly decay and disappear at a constant rate. This can be measured enabling us to calculate the time that has passed since the death of the organism. The drawing will help you understand this process better. 

The “Human Sciences” contribute to our understanding of the physical, social and cultural aspects of human life. 

  • Physical Anthropology: This is the study of human bones, often found in cemeteries, to find out the age and sex of an individual.
  • Palaeopathology: This is the study of ancient diseases by analysing bones.  It can also be used to identify the cause of death. 
  • Ethnoarchaeology: The study of traditional lifestyles that can be applied to the study of ancient societies. 
  • Numismatics: The study of coins. This gives us information about past economies and trade. It is also very useful for dating. 
  • Epigraphy: The study of inscriptions made on hard surfaces (stone, metal, ceramic). It can provide information on past societies, economy, religion and chronology. 
  • Analysis of written sources: The analysis of ancient texts (literature, historical, etc…) can provide information on past societies, often on aspects that archaeology cannot – eg beliefs, fashion, historical events, etc. 
Bandeja Carbono 14

Radiocarbon Dating (C-14)

Carbon 14 atoms are produced in the atmosphere and are absorbed by all living things. They are initially absorbed by plants through photosynthesis, later by herbivore animals eating the plants, and then by carnivores feeding on the herbivores. Finally they are absorbed by people who eat both animals and plants. Therefore, all living things end up having C-14 atoms in their bodies.

Bandeja Carbono 14
EXERCISE ICON

NEANDHERTAL AND HOMO SAPIENS SAPIENS

In the second educational interactive there are two skulls. The one on the left is of a Neanderthal man and the one on the right belongs to a modern man (a Cro-Magnon or Homo Sapiens Sapiens). Download the following exercise and identify eight of its characteristics by contrasting them.

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Cráneo de hombre de Cromagnom
Craneo MARQ

THIRD EDUCATIONAL INTERACTIVE

In this section, we have grouped together the various disciplines associated with the study of archaeological objects and materials known as “archaeometry.” The scientific methods used depend on the nature of the objects being analysed. The aim is to find out more about their composition, provenance and date. 

Traceology is another associated method of analysing archaeological objects. It is the analysis of wear marks on stone, bone, or metal tools using a microscope. This study can provide a lot of information on what the objects were used for.  

Bandeja Arqueometria
Bandejas didácticas
EXERCISE ICON

Match these archaeological objects with the disciplines used to study them.

Download the last exercise in this room and link with arrows a list of archaeological objects with the scientific disciplines that study them specifically.

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