Michigan Fossils Side by Side

Total Page:16

File Type:pdf, Size:1020Kb

Michigan Fossils Side by Side MMiicchhiiggaann FFoossssiillss A2 - BRACHIOPOD, B2 - CRINOID pieces, A1 - BRACHIOPOD, B1 - CORAL or CHAIN invertebrate - invertebrate - invertebrate - CORAL, invertebrate - Mucrospifier profundus - Megistocrinus sp. ? - Pentamerus sp. - Cordell Halysites sp. - Cordell Silica formation - Alpena limestone - dolomite - Silurian age - dolomite - Silurian age - Devonian age - Devonian age - Alpena Chippewa Co. - 65 mm, Chippewa Co. - 110 mm, Washtenaw Co. - 50 mm, Co. - 30 mm (lower right) internal cast or steinkern siliceous replacement - calcite replacement - R. , calcite replacement - - R. Elowski R. Milstein Milstein GSD B4 - CORAL or A4 - CORAL or B3 - SNAIL or COLONIAL CORAL A3 - TRILOBITE, COLONIAL CORAL, GASTROPOD, Petoskey Stone, invertebrate - Phacops invertebrate - invertebrate - genus not invertebrate - rana - Silica formation - Syringopora sp. - Cordell determined - Cordell Hexagonaria percarinata Devonian age - dolomite - Silurian age - dolomite - Silurian age - - Alpena Limestone - Washtenaw Co. - 70 mm, s Chippewa Co. - 125 mm, s Chippewa Co. - 75 mm, Devonian age - calcite replacement - S. siliceous replacement - l internal cast or steinkern Charlevoix Co. - 200 mm, Wilson l R. Milstein - GSD calcite replacement - R. i i Milstein s s D1 - BANDED IRON C1 - MASTODON Tooth, C2 - EUCARYOTIC algae FORMATION (BIF), from D2 - PLANT root section, s vertebrate - Mammut filaments, plant - s fossils - result of plant - Stigmaria, genus americanum - Glacial Grypania spiralis - Grypania and others - not determined - Saginaw deposit - Quaternary age Negaunee Iron Formation Banded Iron Formation - Formation - o - 200 mm long, the - Precambrian age - o Precambrian age - Pennsylvanian age - “Michigan State Fossil” - Marquette Co. - large Marquette Co. - 600 mm, Eaton Co. - 150 mm in Central Michigan loop about 20 mm , F from the rock walkway at diameter, internal cast - F University Rowe Museum oldest macrofossil - GSD the - Eddy Discovery T. Godbold Center n n C3 - FISH plate, D3 - Kona Dolomite, plant D4 - ALGAL stromatolite, a vertebrate - genus not a - Algal in origin - Kona plant - Collenia undosa - determined - Alpena C4 - Septarian nodule - Formation - Precambrian Copper Harbor Limestone - Devonian pseudo fossil - - Ottawa g g age - Marquette Co. - 150 Conglomerate - age - Alpena Co. - 200 Co. - 75 mm, Looks like a by 200 mm, Precambrian age, 1,100 - i mm at widest point, fossil, it is not. - S. Wilson i metamorphosed to a Keweenawan Co. - 100 calcite replacement - S. marble - GSD mm, - S. Wilson Wilson h h c c i E2 - CORAL or i F1 - BRYOZOAN, F2 - CLAM or E1 - CRINOID, COLONIAL CORAL, invertebrate - PELECYPOD, invertebrate - invertebrate - Favosites Sulcoretepora deissi - invertebrate - Megalomus Megistocrinus concava - sp. - Alpena Limestone - Silica formation - canadensis - Cordell Thunder Bay limestone - M Devonian age - M Devonian age - dolomite - Silurian age - Devonian age - Alpena Charlevoix Co. - 100 mm Washtenaw Co. - 25 mm, Chippewa Co. - 60 x 75 Co. - 30 mm, calcite (shown), siliceous calcite replacement - S. mm, internal cast or replacement - S. Wilson replacement - R. Reszka Wilson steinkern - GSD E3 - BRACHIOPOD, E4 - CEPHALOPOD, F3 - CORAL or F4 - STROMATOPOROID, invertebrate - invertebrate - COLONIAL CORAL, invertebrate - genus not Mucrospifler mucronatus Michelinoceras sp. - invertebrate - Favosites determined - Alpena - Silica formation - Ogontz limestone - sp. - Cordell dolomite - Limestone - Devonian Devonian age - Ordovician age - Alger Silurian age - Chippewa age - Charlevoix Co. - Washtenaw Co. - 90 mm, Co. - 100 mm, internal Co. - 70 mm, siliceous 125 mm, calcite calcite replacement - R. cast or steinkern - R. replacement - GSD replacement - GSD Milstein Milstein .
Recommended publications
  • Silurian Rugose Corals of the Central and Southwest Great Basin
    Silurian Rugose Corals of the Central and Southwest Great Basin GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 Silurian Rugose Corals of the Central and Southwest Great Basin By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 A stratigraphic-paleontologic investigation of rugose corals as aids in age detern2ination and correlation of Silurian rocks of the Great Basin with those of other regions UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600082 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price $2.15 (paper cover) Stock Number 2401-00363 CONTENTS Page Page Abstract--------------------------------------------------------------------------- 1 Systematic and descriptive palaeontology-Continued Introduction -------------------------------------------------------------------- 1 Family Streptelasmatidae-Continued Purpose and scope of investigation-------------------------------­ 1 Dalmanophyllum ------------------------------------------------- 32 History of investigation ----------------------------------------------­ 1 Family Stauriidae ------------------------------------------------------- 32 Methods of study-------------------------------------------------------­ 2 Cyathoph y llo ides-------------------------------------------------- 32 Acknowledgments------------------------------------------------------- 4 Palaeophyllum
    [Show full text]
  • Michigan Geologic Time Line List Michigan Rocks: Student No
    Michigan Geologic Time Line List Michigan Rocks: www.educ.msu.edu/michiganrocks Student No. Event Age Geologic Time Name Division 1. Modern Humans .01 (10,000 Holocene years) 2. Ice Age Begins; Glaciers 2 million years Pleistocene cover all of Michigan; Great ago Lakes carved out by Glaciers 3. First Humans 4.5 million Pliocene years ago 4. First Horses 40 million years Eocene ago 5. Last Dinosaurs 65 million years Cretaceous/Tertiary ago Boundary 6. First Flowering Plants 100 million Cretaceous years ago 7. First Birds 150 million Jurassic years ago 8. Redbeds (reddish 145 million Jurassic sandstones and shales) years ago deposited at the end of the Michigan Basin 9. First Mammals 215 million Triassic years ago 10. First Conifer Trees 230 million Triassic years ago 11. First Dinosaurs 240 million Triassic years ago 12. Last Trilobites 250 million Permian/Triassic years ago Boundary 13. Swampland in Lower 290 million Pennsylvanian Peninsula and eastern years ago Upper Peninsula, Michigan Basin. Peat deposits. Also oil and gas deposits 14. First Reptiles 300 million Pennsylvanian years ago 15. Gypsum and Limestone 320 million Mississippian deposited in shallow seas in years ago Lower Peninsula and eastern Upper Peninsula – Michigan Basin 16. First Sharks 350 million Devonian years ago Student No. Event Age Geologic Name Time Division 17. Hexagonaria coral deposits 360 million years Devonian (becomes MI state fossil aka ago Petosky Stone) in Michigan Basin 18. First Amphibians 370 million years Devonian ago 19. First Insects 400 million years Devonian ago 20. First Land Plants 420 million years Ordovician ago 21.
    [Show full text]
  • University of Michigan University Library
    CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL.23, NO.5, p. 81-91, (4 pls.) JUNE 19, 1970 CORALS OF THE TRAVERSE GROUP OF MICHIGAN PART 13, HEXAGONARIA ERWIN C. STUMM MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: ROBERTV. KESLING The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48104. VOLS.2-22. Parts of volumes may be obtained if available. Price lists available upon inquiry. 1. The rodents from the Hagerman local fauna, Upper Pliocene of Idaho, by Richard J. Zakrzewski. Pages 1-36, with 13 text-figures. 2. A new brittle-star from the Middle Devonian Arkona Shale of Ontario, by Robert V. Kesling. Pages 37-51, with 6 plates and 2 text-figures. 3. Phyllocarid crustaceans from the Middle Devonian Silica Shale of northwestern Ohio and southeastern Michigan, by Erwin C. Stumm and Ruth B. Chilman. Pages 53-71, with 7 plates and 4 text-figures. 4. Drepanaster wrighti, a new species of brittle-star from the Middle Devonian Arkona Shale of Ontario, by Robert V. Kesling. Pages 73-79, with 2 plates.
    [Show full text]
  • The Petoskey Stone Oak Land County Earth Science Club March 2013
    The Petoskey Stone Oak land County Earth Science Club March 2013 www.OCESC.com March Program- Native Nations happens as you push and burnish the bezel. Dwight Keith will show his collection But when setting a stone with corners, the Club Meeting of Native American artifacts. tendency is to push the long sides of the March 6th bezel down first. No compression occurs 7:30 along the sides, and all excess metal is left Organizer for at the corners. Compressing everything Board Meeting Programs/Refreshments Needed there is difficult. Often the only way to Our Club needs an organizer for remove the extra metal at the corner is to 6:30 programs and refreshments. Please make a saw cut and fold the two sides in to consider volunteering- see Dwight touch. Keith or any club officer. If you want a smooth bezel all around the corners, the simple solution is set the April Auction Preparation corners of the bezel first. Then push in and We look forward to the April Auction, burnish the sides. In this way the necessary and now is the time to get ready for it. compression is distributed along the length Beginning Thursday, Feb. 14, we'll of all sides and not forced to occur at the look over minerals, pick out the best corners. With the corners set first, the top and get them ready. edge of the bezel can easily be compressed Come, help us. We work from 1:30pm along the sides. to about 4:00 or whatever time you can help. We will do this for 3-4 Cheaper & Better Pickle weeks.
    [Show full text]
  • CNIDARIA Corals, Medusae, Hydroids, Myxozoans
    FOUR Phylum CNIDARIA corals, medusae, hydroids, myxozoans STEPHEN D. CAIRNS, LISA-ANN GERSHWIN, FRED J. BROOK, PHILIP PUGH, ELLIOT W. Dawson, OscaR OcaÑA V., WILLEM VERvooRT, GARY WILLIAMS, JEANETTE E. Watson, DENNIS M. OPREsko, PETER SCHUCHERT, P. MICHAEL HINE, DENNIS P. GORDON, HAMISH J. CAMPBELL, ANTHONY J. WRIGHT, JUAN A. SÁNCHEZ, DAPHNE G. FAUTIN his ancient phylum of mostly marine organisms is best known for its contribution to geomorphological features, forming thousands of square Tkilometres of coral reefs in warm tropical waters. Their fossil remains contribute to some limestones. Cnidarians are also significant components of the plankton, where large medusae – popularly called jellyfish – and colonial forms like Portuguese man-of-war and stringy siphonophores prey on other organisms including small fish. Some of these species are justly feared by humans for their stings, which in some cases can be fatal. Certainly, most New Zealanders will have encountered cnidarians when rambling along beaches and fossicking in rock pools where sea anemones and diminutive bushy hydroids abound. In New Zealand’s fiords and in deeper water on seamounts, black corals and branching gorgonians can form veritable trees five metres high or more. In contrast, inland inhabitants of continental landmasses who have never, or rarely, seen an ocean or visited a seashore can hardly be impressed with the Cnidaria as a phylum – freshwater cnidarians are relatively few, restricted to tiny hydras, the branching hydroid Cordylophora, and rare medusae. Worldwide, there are about 10,000 described species, with perhaps half as many again undescribed. All cnidarians have nettle cells known as nematocysts (or cnidae – from the Greek, knide, a nettle), extraordinarily complex structures that are effectively invaginated coiled tubes within a cell.
    [Show full text]
  • Geology of Michigan and the Great Lakes
    35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed.
    [Show full text]
  • March 2020 Meetings and Field Trips Cancelled Until Further Notice Due to Covid-19 Concerns
    Daisy Mountain Rockchips The purpose of Daisy Mountain Rock & Mineral Club is to promote and further an interest in geology, mineralogy, and lapidary arts, through education, field experiences, public service, and friendship. VOLUME 5, ISSUE 3 MARCH 2020 MEETINGS AND FIELD TRIPS CANCELLED UNTIL FURTHER NOTICE DUE TO COVID-19 CONCERNS A garden of corals in the now-buried (by lava) Kapoho Tidepools, Pahoa, Hawaii. This photo illustrates the colors missing from the fossil record. And it displays the potential growth forms -- many of which are related to the amount of turbulence in the water. Given species may be robust and massive in turbulent environments, and more delicately branching in quiet. Photo by Susan Celestian Daisy Mountain Rockchips March 2020 2 FOSSILS: PART V Kingdom: Animalia GRAPHITE Phylum: Cnidaria By Susan Celestian By Susan Celestian Graphite was known as plumbago, since 1739, but More complex than Porifera (sponges), the phylum was named for the Greek graphein (“to write”) by Cnidaria includes corals, sea anemones, sea Abraham Gottlieb Werner in 1789. It is one of pens, jellyfish, box jellies, hydrozoa (which include four minerals composed of carbon, the others the Portuguese Man O’War), stalked jellyfish, and being: diamond, chaoite, and lonsdaleite. other lesser known groups and species. Of these, Diamond -- the hardest natural substance known by far the majority in the fossil record are the on Earth -- has the same composition (but different corals, because they include species that create a crystal structure) as Graphite -- one of the softest hard calcium carbonate structure; while the others natural substances. are largely soft-bodied with no hard parts.
    [Show full text]
  • Life in a Northern Town Protecting Our Land
    LIFE IN A NORTHERN TOWN Why Emmet County? PROTECTING OUR LAND Enjoy Our Public Recreational Properties SUPPORT FOR BUSINESS Living and Working REDISCOVER THE PLEASURES OF AIR TRAVEL Pellston Regional Airport Pellston Regional Airport is a pleasant surprise in many ways. An award-winning terminal, short lines, free parking, convenient business amenities and superlative staff remind you of the golden age of air travel. And 21st century conveniences—commercial air service with daily flights to Detroit Metro, free wireless Internet access and on-site dining—make Pellston Regional a hallmark in the industry. 231.539.8441 pellstonairport.com North U.S. 31· Pellston, Michigan 49769 Quality Roofing & Seamless Gutter Moran Construction, Inc. 231.535.2175 • Seamless gutters • 20 year warranty • 1/2 round copper • Polyurethane • Seamless metal roofing Foam Spray Gun • Gutter guards (Closed Cell Spray Foam Insulation “Highest Rating”) • Cleaning & repairs • Energy Star Program • Professional installation • FREE ESTIMATE • Licensed & insured www.greatlakesbuilding.net COMMERCIAL • RESIDENTIAL • INDUSTRIAL PETOSKEY’SPETOSKEY’S NEWESTNEWEST luxuryhotelluxuryhotel U All room types for families, honeymoons, bridal showers or bachelor/bachelorette parties U 1,000 sq. ft. Conference Room for Bridal Showers, Bridesmaids’ Luncheons or Rehearsal Dinners U Terrace overlooking beautiful Bear River Valley U Limousine service available within Petoskey area for hotel guests. 1751 US 131 SOUTH, PETOSKEY | 888.497.0105 | [email protected] Custom Wood and Log Homes Hunting and Fishing Camps MACKINAW CITY CHAMBER OF COMMERCE Harbor Springs, Michigan We’ve got 231 348 2684 phone 231 348 7079 fax an experience darntonbuilders.com for every [email protected] season. “Integrity, trust, and delivering mackinawchamber.com what we promise.” 888-455-8100 - Richard Darnton ! " # $ %& ' ( #) ! " # $ *&+( ,--.
    [Show full text]
  • Paleozoic Corals of Alaska
    Paleozoic Corals of Alaska Geologic and Paleogeographic Setting of Paleozoic Corals in Alaska Ordovician, Silurian, and Devonian Corals of Alaska Carboniferous Corals of Alaska A Preliminary Report Stratigraphic Distribution of Permian Corals in Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 823-A, B, C, D Paleozoic Corals of Alaska Geologic and Paleogeographic Setting of Paleozoic Corals in Alaska By MICHAEL CHURKIN, JR. Ordovician, Silurian, and Devonian Corals of Alaska By WILLIAM A. OLIVER, JR., CHARLES W. MERRIAM, and MICHAEL CHURKIN, JR. Carboniferous Corals of Alaska A Preliminary Report By AUGUSTUS K. ARMSTRONG Stratigraphic Distribution of Permian Corals in Alaska By CHARLES L. ROWETT GEOLOGICAL SURVEY PROFESSIONAL PAPER 823-A, B, C, D UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1975 UNITED STATES DEPARTMENT OF THE INTERIOR STANLEY K. HATHAWAY, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Main entry under title: Paleozoic corals of Alaska. (Geological Survey professional paper ; 823) CONTENTS: Churkin, M. Jr. Geologic and paleogeographic setting of Paleozoic corals in Alaska. Oliver, W. A. Jr., Merriam, C. W. and Churkin, M., Jr. Ordovician, Silurian, and Devonian corals of Alaska, [etc.] Includes bibliographies and indexes. Supt. of Docs, no.: I 19.16:823-A,B,C,D 1. Corals, Fossil. 2. Paleontology Paleozoic. 3. Paleiontology Alaska. I. Churkin, Michael, 1932- II. Series: United States. Geological Survey. Professional paper ; 823. QE778.P34 563'.6'09798 75-619102 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02666-0 CONTENTS [The letters in parentheses preceding the titles are those used to designate the chapters] Page (A) Geologic and paleogeographic setting of Paleozoic corals in Alaska, by Michael Churkin, Jr.
    [Show full text]
  • The Petoskey Stone Some History, Lore and Facts About the "Petoskey Stone"
    The Petoskey Stone Some history, lore and facts about the "Petoskey Stone" Wouldn't it be great if rocks could talk? For example, Today, Petoskey is a growing city with all of the through legend and facts, a Petoskey Stone could tell comforts of modern life and an appreciation of the past. you much about Michigan's history and geology. This is where Petoskey Stones are found. For those who look, Petoskey Stones are along the beaches, inland in Legend and history are often intertwined. Such is the gravel deposits, and sold in gift shops. case with the Petoskey Stone. The name Petoskey Stone likely came about because it was found and sold as The most often asked question is, "What is a Petoskey a souvenir from the Petoskey area. The name Petoskey Stone?" A Petoskey is a fossil colonial coral. These appears to have originated late in the 18th century. Its corals lived in warm shallow seas that covered Michigan roots stem from an Ottawa Indian legend. According to during Devonian time, some 350 million years ago. legend, a descendant of French nobility named Antoine Carre visited what is now the Petoskey area and became Almost a century after the founding of Petoskey, on a fur trader with the John Jacob Astor Fur Company. June 28, 1965, Governor George Romney signed a bill In time, he met and married an Ottawa Indian princess. that made the Petoskey Stone Michigan's official State Carre became known to the Indians as Neatooshing. Stone. It was fitting that Miss Ella Jane Petoskey, the Eventually he was adopted by the tribe and was made only living grand-child of Chief Petosegay, was present chief.
    [Show full text]
  • Read Ebook {PDF EPUB} Petoskey Stones by Lois Santalo Hello, Sign In
    Read Ebook {PDF EPUB} Petoskey Stones by Lois Santalo Hello, Sign in. Account & Lists Account Returns & Orders. Try Prime PETOSKEY STONES. by Lois Wells Santalo. Book Cover & Preview Text × Formats. Softcover. $18.95. E-Book. $6.00. Softcover. $18.95. Other Books By Author Night of the Humpbacked Moon Lois Wells Santalo $19.95 The House of Music Lois Santalo $15.95 ... AbeBooks.com: PETOSKEY STONES (9780595348589) by Santalo, Lois and a great selection of similar New, Used and Collectible Books available now at great prices. Buy Petoskey Stones by Lois Wells Santalo online at Alibris. We have new and used copies available, in 1 editions - starting at $1.99. Shop now. Find many great new & used options and get the best deals for Petoskey Stones by Lois Santalo (2005, Trade Paperback) at the best online prices at eBay! Free shipping for many products! Petoskey Stones by Lois Wells Santalo, unknown edition, Petoskey Stones (9780595348589).pdf writen by Lois Wells Santalo: World War II is finally over and woman's role in society has undergone a drastic change. Delia Eloise Kingsley confronts a new marriage with a man she does not love, while her cousin, Della "Weezy" Ward, pursues a writi Buy Petoskey Stones by Lois Wells Santalo from Waterstones today! Click and Collect from your local Waterstones or get FREE UK delivery on orders over £25. Amazon.in - Buy Petoskey Stones book online at best prices in india on Amazon.in. Read Petoskey Stones book reviews & author details and more at Amazon.in. Free delivery on qualified orders. Hello Select your address Best Sellers Today's Deals New Releases Electronics Books Customer Service Gift Ideas Home Computers Gift Cards Subscribe and save Coupons Sell Petoskey Stones 296.
    [Show full text]
  • Our State Symbols
    DETROIT FREE PRESS | WWW.YAKSCORNER.COM THURSDAY, MAY 16, 2002 3 Our state symbols f the Petoskey stone could stone, which might better have was a vertebrate, or animal talk, it would tell the story been named the state with a backbone.) of a shallow, sunny sea that invertebrate fossil because In the early part of its life, I PHOTOS BY MARY SCHROEDER once covered what now is that’s what it is. (The new “Hexagonaria looked like a little Michigan and teemed with state fossil, the mastodon, jellyfish,” said Wilson. Mike Mayse, manager of the Cemex quarry in Charlevoix, finds thousands, perhaps “These little buggers some Petoskey stones for the Yak. Make that Petoskey rocks! millions, of coral colonies. were floating anywhere “It was like the Great they could and attaching Barrier Reef,” said Steve to anything hard that that set off to start new are scattered in the cake’s Wilson, a state geologist, they could to continue the colonies. upper layers, “like sprinkles on comparing the little-known growth of the coral.” “Their strength was in being frosting,” said Wilson. But extinct reef to Australia’s Once they had gripped able to link themselves there were plenty in the middle famous one. something hard, such as together,” said Wilson. “They of the cake, too, 41 feet below “I don’t know how long it a rock, they grew upwards, started as one and divided, the lake’s surface. stretched, but these building little tubes as like branches on a tree.” “You trip over them in the critters — fossil corals they ascended.
    [Show full text]