Fossils are the preserved remains or traces of ancient organisms. They are usually found in sedimentary rocks, which are formed when sediments containing remains are buried over time. Fossils form when an organism is buried rapidly in sediment before it can fully decay. The sediment hardens to rock and preserves a record of the organism. Index fossils are fossils used to date rock layers because they existed for a short, well-defined period of time. Nummulites are coin-shaped fossils that were commonly found in the Pyrenees mountains, indicating the presence of Tertiary-era sedimentary rocks formed during the Alpine orogeny.
Microfossils are very small remains of organisms 0.001 mm (1 micron) to 1 mm, that require magnification for study.
They are abundant, can be recovered from small samples.
Provide the main evidence for organic evolution through the time
They classified into two groups:
Organic-walled; Acritarchs, Dinoflagellate, Spores and Pollen grains … etc.
Foraminifera Each chamber interconnected by an opening (foramen) or several openings (foramina).
Known from Early Cambrian through to recent times, and has reached its acme during the Cenozoic.
Have a wide environmental range from terrestrial to deep sea and from polar to the tropical region.
Depending on the species, the shell may be made of organic compounds, sand grains and other particles cemented together, or from crystalline calcite.
Inorganic walled; Diatoms, Silicoflagellates, Ostracods, Conodonts, and Foraminifera
Brief description on Phylum Brachiopods with general terms used for Paleontology.
Structure paleoecology, geography, morphology.
And also easily understandable as since it discuss only specific terms only.
Grade 8 Integrated Science Chapter 12 Lesson 1 on relative-age dating of fossils and rock layers. This lesson explains how scientists use rock layers to determine a age of a rock or fossil compared to others. The goal of this lesson is for students to be able to correctly order rock layers by age and to know the different disconformities and nonconformities.
Microfossils are very small remains of organisms 0.001 mm (1 micron) to 1 mm, that require magnification for study.
They are abundant, can be recovered from small samples.
Provide the main evidence for organic evolution through the time
They classified into two groups:
Organic-walled; Acritarchs, Dinoflagellate, Spores and Pollen grains … etc.
Foraminifera Each chamber interconnected by an opening (foramen) or several openings (foramina).
Known from Early Cambrian through to recent times, and has reached its acme during the Cenozoic.
Have a wide environmental range from terrestrial to deep sea and from polar to the tropical region.
Depending on the species, the shell may be made of organic compounds, sand grains and other particles cemented together, or from crystalline calcite.
Inorganic walled; Diatoms, Silicoflagellates, Ostracods, Conodonts, and Foraminifera
Brief description on Phylum Brachiopods with general terms used for Paleontology.
Structure paleoecology, geography, morphology.
And also easily understandable as since it discuss only specific terms only.
Grade 8 Integrated Science Chapter 12 Lesson 1 on relative-age dating of fossils and rock layers. This lesson explains how scientists use rock layers to determine a age of a rock or fossil compared to others. The goal of this lesson is for students to be able to correctly order rock layers by age and to know the different disconformities and nonconformities.
La educación bilingüe en España y en EuropaIsaac Buzo
Presentación utilizada durante la ponencia "La educación bilingüe en España y en Europa" celebrado en el marco del curso sobre "Didácticas de Materias no lingüísticas para Secciones Bilingües" del CPR de Mérida. Noviembre de 2011.
MORPHOLOGY AND SIGNIFICANCE OF CONODONT (group-D).pptxKuki Boruah
Conodonts are marine organism ranging from Cambrian to Triassic periods, having a long wormlike body, numerous small teeth and a pair of eyes.
It is now believed as the earliest vertebrate and now it is an extinct group of organism.
First identified by the LATVIAN embryologist and palaeontologist Christian Pander in 1856.
Conodonts are most frequently occuring fossil in marine Sedimentary Rocks.
Size of Conodonts commonly in between 200 microns and 5 millimetres.
The preserved color varying from translucent and colorless through light brown to black.
This slide presentation aims to help teachers and students in studying biodiversity and evolution. It consists of images, definition of terms all related to biodiversity and evolution.
Educar para Ser
Vivencias de una escuela activa
Autor: Wild Rebeca
Educar para Ser. No tardamos mucho en darnos cuenta de que, si se quiere que un niño se desarrolle según su ley interior, toda evolución está relacionada con necesidades que deben ser satisfechas. La "escuela activa" valora el cuidado sistemático de procesos de aprendizaje capaces de renovarse.
Fruto de un innovador proyecto educativo, vivido en el seno de la familia y de la comunidad "Educar para ser" explica a padres y maestros cómo crear un ambiente en el que los niños crezcan llenos de curiosidad y seguros de sí mismos y de su entorno.
Al permitirles que experimenten el mundo y lo transformen de un modo que tenga sentido para ellos, el adulto se compromete a un aprendizaje continuo y adaptable a las necesidades de los niños para satisfacerlas en la medida de lo posible.
En este sentido, la "escuela activa" es una propuesta: ni se orienta hacia modelos de educación antiautoritaria, ni se inspira en las escuelas tradicionales basadas en la disciplina. En ella, la actividad de los niños es tan importante como la de los adultos. Por un lado, el adulto aprende a respetar las estructuras mentales y emocionales propias de cada uno de los estadios del desarrollo intanfil. El niño, por su parte, experimenta el valor del respeto y aprende a respetarse a sí mismo y a los adultos.
En lugar de imponer un plan educativo fijo y obligatorio para todos, la "escuela activa" valora el cuidado sistemático de procesos de aprendizaje capaces de renovarse. Los datos demuestran claramente que las ventajas de las formas pedagógicas alternativas se mantienen incluso años más tarde, durante los estudios superiores y en la vida familiar y profesional.
By: Marina Járboles, Cristina Alierta and Pilar Ballesteros.
CELL
Cell Theory
Cell scientists
1) Robert Hooke
2) Antony Van Leeuwenhoek
3) Robert Brown
4) Mattias Schleiden
5) Theodor Schwann
6) Rudolph Virchow
History of microscopes
Types of microscopes
Optical and electron microscopes.
Manual para impartir cursos de conducción de bicicletas en los centros educativos de Terrassa.
Los autores son Haritz Ferrando i Xavier Prats
Normalizar el uso de la bicicleta en las ciudades requiere de un importantes esfuerzo de formación a todos los públicos que potencialmente pueden escoger la bicicleta como medio de transporte. El objetivo de este manual es que los jóvenes incorporen la opción de la bicicleta como medio de transporte principal en sus desplazamientos cotidianos y que cuenten, para ello, con los conocimientos y habilidades básicas para hacerlo con seguridad. Existe una versión en catalán y un video del proyecto.
La dipuotación de Albacete está al frente de la edición de esta guía para fomentar la movilidad sostenible y responsable en las escuelas. (Ed Primaria y Secundaria)
Detective de lo nunca observado. La movilidad urbana: El camino escolar
Las autoras son Monterrubio, Pilar; Rubio, Mercedes; Sintes, María (2004). Edita el Ayuntamiento de Segovia. Por medio de fichas l@s chic@s irán dándose cuenta de las características del camino que recorren hacia la escuela y así se convierten en los agentes principales del diseño y construcción de un verdadero camino escolar.
"Un diseño didáctico que pone el acento no en los aspectos relacionados con la seguridad o el urbanismo sino en las experiencias, percepciones y emociones."
2. What is a FossilFossil?
Fossils
(from Latin fossus, literally "having been dug up")
are the preserved remains or traces of
animals, plants, and other organisms from the
remote past.
4. • Why would you not expect to find
fossils in igneous rocks?
• Can you find fossils in metamorphic rocks?
blog.senhordesign.com
5. • Coprolites and icnites are fossils too.
A coprolite is fossilized
animal dung (feces)
Icnites (dinosaurs' footprints)
Enciso-LaRioja-
6. Index fossils
• Index fossilsIndex fossils (also known as guide fossils,
indicator fossils or zone fossils) are fossils used
to define and identify geologic periods (or
faunal stages).
7.
8. Index fossil features
The ideal index fossilsideal index fossils are those that are:
• abundant,
• easy to identify,
• short-lived,
• widely distributed,
• and occur in many types of rocks.
9. Describe howDescribe how fossilsfossils are formed inare formed in
sedimentary rocks…sedimentary rocks…
Check this animated explanation
http://www.bbc.co.uk/sn/prehistoric_life/dinosaurs/making_fossils/makingfossils/index.shtml
http://www.classzone.com/books/earth_science/terc/content/visualizations/es2901/es2901page01.cfm?chapter_no=visualization
10. Describe how fossils are formed in
sedimentary rocks…
http://www.science-graphics.net
13. Do all animals fossilizze?
Most animals did not fossilize;
they simply decayed and were lost from the fossil
record.
Paleontologists estimate that only a small percentage of
the dinosaur genera that ever lived have been or will be
found as fossils.
14. • What important facts can fossils tells us about
sedimentary rocks and the environment in which
they were formed?
• In what ways is the fossil record importance to
science?
blog.senhordesign.com
16. Trilobite
• (meaning "three lobes") Trilobites are a well-
known fossil group of extinct marine arthropods
that form the class Trilobita.
• When trilobites first appeared in the fossil record
they were already highly diverse and
geographically dispersed. Because trilobites had
wide diversity and an easily fossilized
exoskeleton an extensive fossil record was left,
with some 17,000 known species spanning
Paleozoic time.
17.
18. Ammonite
• Ammonites are an
extinct group of marine
invertebrate animals in
the subclass
Ammonoidea of the class
Cephalopoda.
20. Belemnites
• Belemnites were numerous during the
Jurassic and Cretaceous periods
Belemnites are the internal shells of an extinct
type of cephalopod mollusc related to modern
octopus and squid.
21. Nummulite
• A nummulite is a large lenticular fossil,
characterized by its numerous coils,
subdivided by septa into chambers. They are
the shells of the fossil and present-day marine
protozoan
22. The name "Nummulites" is a diminutive form of the Latin nummulus meaning "little
coin", a reference to their shape
23. Nummulite
• They are common in Tertiary marine rocks,
particularly around the Mediterranean.
http://geology.com/publications/lyell/ch16.shtml
24. Which one is older?
http://www.physicsforums.com/showthread.php?t=63524
25. Which one is older?
http://www.physicsforums.com/showthread.php?t=63524
26. Which one could we easily find in the
Pyrenees?
http://www.physicsforums.com/showthread.php?t=63524
27. Which one could we easily find in the
Pyrenees?
http://www.physicsforums.com/showthread.php?t=63524
28. Which one could we easily find in the
Pyrenees?
http://www.physicsforums.com/showthread.php?t=63524
Why?Why?
29. Which one could we easily find in the
Pyrenees?
http://www.physicsforums.com/showthread.php?t=63524
Why?
Tertiary –Tertiary –
Alpine orogeny –Alpine orogeny –
PyreneesPyrenees
30. • http://en.wikipedia.org/
• http://www.nhm.ac.uk/nature-online/earth/fossils/fossil-folklore/fossil_types/
• http://wiki.answers.com/Q/What_are_three_characteristics_of_a_good_index_fossil
• http://www.enchantedlearning.com/subjects/dinosaurs/dinofossils/Fossilhow.html
• http://www.bbc.co.uk/sn/prehistoric_life/dinosaurs/making_fossils/makingfossils/index.shtml
• Icnite picture at Enciso La Rioja, from
• http://www.vallenajerilla.com/berceo/rioja-abierta/pangea/anteshistoria.htm