Difference between revisions of "AY Honors/Fossils/Answer Key 2/es"
(Updating to match new version of source page) |
(Created page with "</noinclude> <!-- a. Geología -->") |
||
Line 1: | Line 1: | ||
{{HonorSubpage}} | {{HonorSubpage}} | ||
+ | |||
{{#vardefine:reqpage|{{#titleparts:{{PAGENAME}}|2}}/Requirements 2}} | {{#vardefine:reqpage|{{#titleparts:{{PAGENAME}}|2}}/Requirements 2}} | ||
− | <section begin="Body" /> | + | <section begin="Body" /> |
+ | |||
{{ansreq|page={{#var:reqpage}}|num=1}} | {{ansreq|page={{#var:reqpage}}|num=1}} | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
− | <!-- 1. | + | <!-- 1. Proporcionar una breve definición de cada uno de los siguientes términos: --> |
− | + | <noinclude></noinclude> | |
− | {{ | + | {{ansreq|page={{#var:reqpage}}|num=1a}} |
+ | <noinclude></noinclude> | ||
+ | <!-- a. Geología --> | ||
− | + | <noinclude></noinclude> | |
− | + | {{CloseReq}} <!-- 1a --> | |
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | {{ | ||
− | {{ | + | {{ansreq|page={{#var:reqpage}}|num=1b}} |
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- b. Fossils --> | ||
+ | Fossils are the mineralized or otherwise preserved remains or traces (such as footprints) of animals, plants, and other organisms. | ||
+ | </div> | ||
− | + | <div lang="en" dir="ltr" class="mw-content-ltr"> | |
− | + | <noinclude> | |
− | {{ | + | </div></noinclude> |
+ | {{CloseReq}} <!-- 1b --> | ||
− | {{ | + | {{ansreq|page={{#var:reqpage}}|num=1c}} |
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- c. Catastrophism --> | ||
+ | </div> | ||
− | {{ | + | <div lang="en" dir="ltr" class="mw-content-ltr"> |
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | {{CloseReq}} <!-- 1c --> | ||
+ | Catastrophism is the idea that Earth has been affected by sudden, short-lived, violent events that were sometimes worldwide in scope. | ||
− | {{ | + | {{ansreq|page={{#var:reqpage}}|num=1d}} |
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- d. Paleobotany, Paleontology --> | ||
+ | Paleobotany is the branch of paleontology or paleobiology dealing with the recovery and identification of plant remains from geological contexts, and their use for the biological reconstruction of past environments. Paleobotany includes the study of terrestrial plant fossils, as well as the study of prehistoric marine photoautotrophs, such as photosynthetic algae, seaweeds or kelp. | ||
+ | </div> | ||
− | + | <div lang="en" dir="ltr" class="mw-content-ltr"> | |
+ | Paleontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils. | ||
+ | </div> | ||
− | <noinclude></noinclude> | + | <div lang="en" dir="ltr" class="mw-content-ltr"> |
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | {{CloseReq}} <!-- 1d --> | ||
{{CloseReq}} <!-- 1 --> | {{CloseReq}} <!-- 1 --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=2}} | {{ansreq|page={{#var:reqpage}}|num=2}} | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
<!-- 2. Tener una breve definición de cada una de las siguientes en su libreta de notas: --> | <!-- 2. Tener una breve definición de cada una de las siguientes en su libreta de notas: --> | ||
− | <noinclude></noinclude> | + | <noinclude> |
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=2a}} | {{ansreq|page={{#var:reqpage}}|num=2a}} | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
Line 46: | Line 73: | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
{{CloseReq}} <!-- 2a --> | {{CloseReq}} <!-- 2a --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=2b}} | {{ansreq|page={{#var:reqpage}}|num=2b}} | ||
− | <noinclude></noinclude><noinclude></noinclude> | + | <noinclude></noinclude><noinclude> |
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | A Graptolite is a fossil colonial animal known chiefly from the Upper Cambrian through the Lower Carboniferous (Mississippian) periods. | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
{{CloseReq}} <!-- 2b --> | {{CloseReq}} <!-- 2b --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=2c}} | {{ansreq|page={{#var:reqpage}}|num=2c}} | ||
− | <noinclude></noinclude><noinclude></noinclude> | + | <noinclude></noinclude><noinclude> |
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
{{CloseReq}} <!-- 2c --> | {{CloseReq}} <!-- 2c --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=2d}} | {{ansreq|page={{#var:reqpage}}|num=2d}} | ||
− | <noinclude></noinclude><noinclude></noinclude> | + | <noinclude></noinclude><noinclude> |
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
{{CloseReq}} <!-- 2d --> | {{CloseReq}} <!-- 2d --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=2e}} | {{ansreq|page={{#var:reqpage}}|num=2e}} | ||
− | <noinclude></noinclude><noinclude></noinclude> | + | <noinclude></noinclude><noinclude> |
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | A mammoth is any species of an extinct genus of proboscidean (elephants and their extinct relatives), often with long curved tusks and, in northern species, a covering of long hair. [[File:Mammoth tusks.jpg|thumb|200px|Mammoth tusks]] | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
{{CloseReq}} <!-- 2e --> | {{CloseReq}} <!-- 2e --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=2f}} | {{ansreq|page={{#var:reqpage}}|num=2f}} | ||
− | <noinclude></noinclude><noinclude></noinclude> | + | <noinclude></noinclude><noinclude> |
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | Pelecypod are molluscs belonging to the class Bivalvia. They typically have two-part shells, with both valves being symmetrical along the hinge line. The class has 30,000 species, including scallops, clams, oysters and mussels. | ||
+ | [[File:Shell Limestone.jpg|thumb|200px|Shell Limestone]] | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
{{CloseReq}} <!-- 2f --> | {{CloseReq}} <!-- 2f --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=2g}} | {{ansreq|page={{#var:reqpage}}|num=2g}} | ||
− | <noinclude></noinclude><noinclude></noinclude> | + | <noinclude></noinclude><noinclude> |
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
{{CloseReq}} <!-- 2g --> | {{CloseReq}} <!-- 2g --> | ||
− | + | {{CloseReq}} <!-- 2 --> | |
− | + | ||
− | + | {{ansreq|page={{#var:reqpage}}|num=3}} | |
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | {{CloseReq}} <!-- | ||
− | |||
− | |||
− | |||
− | {{ansreq|page={{#var:reqpage}}|num= | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
− | < | + | <div lang="en" dir="ltr" class="mw-content-ltr"> |
− | + | The Paleozoic Era is the earliest of three geologic eras of the Phanerozoic eon. The Paleozoic era is defined by evolutionary geologists as spanning from roughly 542 million years ago to roughly 251 million years ago. | |
− | + | </div> | |
− | + | ||
− | + | <noinclude> | |
− | + | ||
− | <noinclude> | + | <div lang="en" dir="ltr" class="mw-content-ltr"> |
− | + | Lying between the Paleozoic and the Cenozoic, Mesozoic means 'middle animals'. It is often called the 'Age of the Dinosaurs'. | |
− | + | </div> | |
− | + | ||
− | + | <div lang="en" dir="ltr" class="mw-content-ltr"> | |
− | + | The Cenozoic Era is the latest of three geologic eras of the Phanerozoic eon. Evolutionary geologists define this era as having started about 65 million years ago, when the age of the dinosaurs ended. | |
− | + | </div> | |
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | < | + | <div lang="en" dir="ltr" class="mw-content-ltr"> |
− | + | The Pleistocene epoch on the evolutionary geologic timescale is the period from 1,808,000 to 11,550 years before present. The Pleistocene epoch had been intended to cover the world's recent period of repeated glaciations, or the Ice Age. | |
− | + | </div> | |
− | |||
− | |||
<noinclude></noinclude> | <noinclude></noinclude> | ||
{{CloseReq}} <!-- 3 --> | {{CloseReq}} <!-- 3 --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=4}} | {{ansreq|page={{#var:reqpage}}|num=4}} | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
Line 136: | Line 180: | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
{{CloseReq}} <!-- 4 --> | {{CloseReq}} <!-- 4 --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=5}} | {{ansreq|page={{#var:reqpage}}|num=5}} | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
Line 142: | Line 187: | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
{{CloseReq}} <!-- 5 --> | {{CloseReq}} <!-- 5 --> | ||
+ | |||
{{ansreq|page={{#var:reqpage}}|num=6}} | {{ansreq|page={{#var:reqpage}}|num=6}} | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
Line 158: | Line 204: | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
{{CloseReq}} <!-- 6 --> | {{CloseReq}} <!-- 6 --> | ||
+ | |||
+ | {{ansreq|page={{#var:reqpage}}|num=7}} | ||
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- 7. Research five fossil ancestors of animals living today. How do the fossil ancestors compare and contrast with modern animals? --> | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | {{CloseReq}} <!-- 7 --> | ||
+ | |||
+ | {{ansreq|page={{#var:reqpage}}|num=8}} | ||
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- 8. Do two of the following: --> | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | |||
+ | {{ansreq|page={{#var:reqpage}}|num=8a}} | ||
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- a. Spend time searching for fossils and attempting to identify them. Bring them in to show your Pathfinder Club. --> | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | {{CloseReq}} <!-- 8a --> | ||
+ | |||
+ | {{ansreq|page={{#var:reqpage}}|num=8b}} | ||
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- b. Make a plant or animal fossil model with plaster, clay or other medium. --> | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | {{CloseReq}} <!-- 8b --> | ||
+ | |||
+ | {{ansreq|page={{#var:reqpage}}|num=8c}} | ||
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- c. Visit a museum where fossils are on display and make a written or oral report of your trip. --> | ||
+ | [[File:Tyrannosaurus rex Stan.jpg|thumb|300px|Tyranasaurus rex]] | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | Most museums of natural history will have a fossil collection, and even small museums are likely to have a few. If you do not know of such a museum in your area, the Internet is your friend. Try searching for "fossil," "museum," and the name of your locality. If you are still unsure, get a list of local museums and call them. They will be happy to tell you if they have fossils on display, and if they do not, they may be able to direct you to a museum that does. Also not all museums are called a museum. The T Rex and some other fossils shown here were photographed at Science World in Vancouver. | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | After the visit, have your Pathfinders either write their reports or present one orally. This would be a great topic for worship during your club's opening exercises, or during a campout. | ||
+ | {{clear}} | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | {{CloseReq}} <!-- 8c --> | ||
+ | {{CloseReq}} <!-- 8 --> | ||
+ | |||
+ | {{ansreq|page={{#var:reqpage}}|num=9}} | ||
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- 9. Make a collection of at least ten different kinds of fossils and label each with its name and geographic location. Classify them as impression, mineralized, trace or preserved organic material. --> | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | Fossils are found in many places where sedimentary rocks, such as claystones, shales, limestones, and sandstones, are exposed. Only certain sedimentary rocks harbored the appropriate environmental conditions to preserve and yield fossils, which are often concentrated along particular bedding planes within the rocks. | ||
+ | </div> | ||
+ | |||
+ | </noinclude> | ||
+ | <!-- 1. Dibujar, fotografiar o hacer una colección de al menos 10 diferentes clases de fósiles y etiquetar cada uno con su nombre y dónde se encuentra. --> | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | {{clear}} | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | {{CloseReq}} <!-- 9 --> | ||
+ | |||
+ | {{ansreq|page={{#var:reqpage}}|num=10}} | ||
+ | <noinclude><div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | </noinclude> | ||
+ | <!-- 10. Prepare a parable or short spiritual lesson based on fossils using what has been learned in this honor. --> | ||
+ | </div> | ||
+ | |||
+ | <div lang="en" dir="ltr" class="mw-content-ltr"> | ||
+ | <noinclude> | ||
+ | </div></noinclude> | ||
+ | {{CloseReq}} <!-- 10 --> | ||
+ | |||
<noinclude></noinclude> | <noinclude></noinclude> | ||
==Referencias== | ==Referencias== | ||
<noinclude></noinclude> | <noinclude></noinclude> | ||
+ | |||
{{CloseHonorPage}} | {{CloseHonorPage}} |
Revision as of 15:32, 27 March 2024
1
1a
1b
Fossils are the mineralized or otherwise preserved remains or traces (such as footprints) of animals, plants, and other organisms.
1c
Catastrophism is the idea that Earth has been affected by sudden, short-lived, violent events that were sometimes worldwide in scope.
1d
Paleobotany is the branch of paleontology or paleobiology dealing with the recovery and identification of plant remains from geological contexts, and their use for the biological reconstruction of past environments. Paleobotany includes the study of terrestrial plant fossils, as well as the study of prehistoric marine photoautotrophs, such as photosynthetic algae, seaweeds or kelp.
Paleontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils.
2
2a
2b
A Graptolite is a fossil colonial animal known chiefly from the Upper Cambrian through the Lower Carboniferous (Mississippian) periods.
2c
2d
2e
2f
Pelecypod are molluscs belonging to the class Bivalvia. They typically have two-part shells, with both valves being symmetrical along the hinge line. The class has 30,000 species, including scallops, clams, oysters and mussels.
2g
3
The Paleozoic Era is the earliest of three geologic eras of the Phanerozoic eon. The Paleozoic era is defined by evolutionary geologists as spanning from roughly 542 million years ago to roughly 251 million years ago.
Lying between the Paleozoic and the Cenozoic, Mesozoic means 'middle animals'. It is often called the 'Age of the Dinosaurs'.
The Cenozoic Era is the latest of three geologic eras of the Phanerozoic eon. Evolutionary geologists define this era as having started about 65 million years ago, when the age of the dinosaurs ended.
The Pleistocene epoch on the evolutionary geologic timescale is the period from 1,808,000 to 11,550 years before present. The Pleistocene epoch had been intended to cover the world's recent period of repeated glaciations, or the Ice Age.
4
5
6
De Historia de Patriarcas y Profetas, p. 98, 99 |
---|
Por doquiera yacían cadáveres de hombres y animales. El Señor no iba a permitir que permaneciesen allí para infectar el aire por su descomposición, y por lo tanto, hizo de la tierra un vasto cementerio. Un viento violento enviado para secar las aguas, las agitó con gran fuerza, de modo que en algunos casos derribaron las cumbres de las montañas y amontonaron árboles, rocas y tierra sobre los cadáveres.
En ese tiempo inmensos bosques fueron sepultados. Desde entonces se han transformado en el carbón de piedra de las extensas capas de hulla que existen hoy día, y han producido también enormes cantidades de petróleo. Con frecuencia la hulla y el petróleo se encienden y arden bajo la superficie de la tierra. Esto calienta las rocas, quema la piedra caliza, y derrite el hierro. |
7
8
8a
8b
8c
Most museums of natural history will have a fossil collection, and even small museums are likely to have a few. If you do not know of such a museum in your area, the Internet is your friend. Try searching for "fossil," "museum," and the name of your locality. If you are still unsure, get a list of local museums and call them. They will be happy to tell you if they have fossils on display, and if they do not, they may be able to direct you to a museum that does. Also not all museums are called a museum. The T Rex and some other fossils shown here were photographed at Science World in Vancouver.
After the visit, have your Pathfinders either write their reports or present one orally. This would be a great topic for worship during your club's opening exercises, or during a campout.
9
Fossils are found in many places where sedimentary rocks, such as claystones, shales, limestones, and sandstones, are exposed. Only certain sedimentary rocks harbored the appropriate environmental conditions to preserve and yield fossils, which are often concentrated along particular bedding planes within the rocks.
10