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Quaternary Environments Quaternary Environments Non-Marine Biological Non-Marine Biological Evidence Evidence
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Quaternary Environments Non-Marine Biological Evidence.

Dec 18, 2015

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Page 1: Quaternary Environments Non-Marine Biological Evidence.

Quaternary EnvironmentsQuaternary EnvironmentsNon-Marine Biological EvidenceNon-Marine Biological Evidence

Page 2: Quaternary Environments Non-Marine Biological Evidence.

Proxy RecordsProxy Records

Macrofossil EvidenceMacrofossil Evidence PackratsPackrats Tree-line fluctuationTree-line fluctuation

Microfossil EvidenceMicrofossil Evidence PollenPollen

InsectsInsects

Page 3: Quaternary Environments Non-Marine Biological Evidence.

Macrofossil EvidenceMacrofossil Evidence

Quantitative analysis of Quaternary plant Quantitative analysis of Quaternary plant macrofossils began in 1957 (West 1957)macrofossils began in 1957 (West 1957)

Seeds, fruits (orchids to coconuts), cones, Seeds, fruits (orchids to coconuts), cones, sporangiasporangia

Leaves, needles, budsLeaves, needles, buds WoodWood

Page 4: Quaternary Environments Non-Marine Biological Evidence.

Macrofossil SeedsMacrofossil Seeds

Page 5: Quaternary Environments Non-Marine Biological Evidence.

Needle Cross SectionNeedle Cross Section

Page 6: Quaternary Environments Non-Marine Biological Evidence.

Macrofossil DiagramMacrofossil Diagram

Page 7: Quaternary Environments Non-Marine Biological Evidence.

PaleoscatologyPaleoscatology

ScatScat Procedure Procedure

BlendBlendScreenScreen

Coprolites AnalysisCoprolites Analysis Can identify food sources and diseaseCan identify food sources and disease

Page 8: Quaternary Environments Non-Marine Biological Evidence.

CuticlesCuticles

Waxy coating that has distinct morphologyWaxy coating that has distinct morphology Stomata: control gas exchangeStomata: control gas exchange Trichomes (leaf hairs)Trichomes (leaf hairs) Cork cells (provide leaf support)Cork cells (provide leaf support) Silica cells (support, discourage foliavores)Silica cells (support, discourage foliavores)

Page 9: Quaternary Environments Non-Marine Biological Evidence.

PhytolithsPhytoliths Production

Silica is deposited in the secondary plant wall of some plants, particularly grasses and occasionally in wood.

Phytoliths most abundant in grasslands and steppes. Disperal

Large fragments move short distances (fragile) small fragments (silt sized) may be distributed by wind.

Preservation Resistant to oxidation, but the silica can be dissolved

by ground-water movement

Page 10: Quaternary Environments Non-Marine Biological Evidence.

Phytolith MorphologyPhytolith Morphology

Page 11: Quaternary Environments Non-Marine Biological Evidence.

Poaceae Zea luxuriens PhytolithPoaceae Zea luxuriens Phytolith

Page 12: Quaternary Environments Non-Marine Biological Evidence.

Poaceae Paspalum lividum PhytolithPoaceae Paspalum lividum Phytolith

Page 13: Quaternary Environments Non-Marine Biological Evidence.

Asteraceae Lipochaeta sp. PhytolithAsteraceae Lipochaeta sp. Phytolith

Page 14: Quaternary Environments Non-Marine Biological Evidence.

PhytolithsPhytoliths

Identification Many plants don't produce phytoliths: only a partial

indication of plants in area Non-related species produce the same types :

dumbbells, saddles, bowls, boats, bottoms Some Taxonomic categories can be recognized:

panicoid, festucoid, chloroid A few forms are diagnostic to species level: e.g.,

maize

Page 15: Quaternary Environments Non-Marine Biological Evidence.

Phytolith MethodsPhytolith Methods

Oxidize sample (boil in HOxidize sample (boil in H22OO22)) Wet sieve (phytoliths silt size)Wet sieve (phytoliths silt size) Flotation (tetrabromoethane, ZnBr2) phytoliths Flotation (tetrabromoethane, ZnBr2) phytoliths

have specific gravity of 1.5-2.3, quartz 2.65have specific gravity of 1.5-2.3, quartz 2.65

Page 16: Quaternary Environments Non-Marine Biological Evidence.

Wood AnatomyWood Anatomy

Can identify wood to the species or genus Can identify wood to the species or genus levellevel Cell structureCell structure PitsPits TracheidsTracheids PoresPores Resin ductsResin ducts

Page 17: Quaternary Environments Non-Marine Biological Evidence.

Wood AnatomyWood Anatomy

Page 18: Quaternary Environments Non-Marine Biological Evidence.

TreelineTreeline

Upper TreelineUpper Treeline Temperature controlledTemperature controlled Dating wood from tree above current treelineDating wood from tree above current treeline Arctic brown paleosols beneath recent Arctic brown paleosols beneath recent

SpodosolsSpodosols Lower TreelineLower Treeline

Moisture controlledMoisture controlled Packrat MiddensPackrat Middens

Page 19: Quaternary Environments Non-Marine Biological Evidence.

KrummholzKrummholz

Prostrate stunted vegetationProstrate stunted vegetation Protected by snow packProtected by snow pack Can grow above present treelineCan grow above present treeline Technically a different genetic species of a plant Technically a different genetic species of a plant

that has stunted growth, but broadly used for that has stunted growth, but broadly used for environmentally stunted treesenvironmentally stunted trees

Page 20: Quaternary Environments Non-Marine Biological Evidence.

Flagged leaders standing out Flagged leaders standing out from a Krummholz mattfrom a Krummholz matt

Page 21: Quaternary Environments Non-Marine Biological Evidence.

©Tom Kloster 2001: http://www.splintercat.org/JeffParkRidge/ParkRidgeImages/

Page 22: Quaternary Environments Non-Marine Biological Evidence.

©Tom Kloster 2001: http://www.splintercat.org/JeffParkRidge/ParkRidgeImages/

Page 23: Quaternary Environments Non-Marine Biological Evidence.

http://patti.tensegrity.net/album/moraine/display/trees.html

Page 24: Quaternary Environments Non-Marine Biological Evidence.

Problems with Treeline StudiesProblems with Treeline Studies

Incomplete fossil record (highest elevation trees Incomplete fossil record (highest elevation trees may not have been found)may not have been found)

Elevation of mountain summits restrict how high Elevation of mountain summits restrict how high treeline could be recordedtreeline could be recorded

Present treeline is hard to determinePresent treeline is hard to determine Disturbances can affect tree line (fire, grazing, Disturbances can affect tree line (fire, grazing,

avalanches, wind abrasion, insects)avalanches, wind abrasion, insects) Lag time in response to climate changesLag time in response to climate changes

Advance faster than retreatAdvance faster than retreat

Treeline may be affected by isostatic upliftTreeline may be affected by isostatic uplift

Page 25: Quaternary Environments Non-Marine Biological Evidence.

Treeline Fluctuations, SwedenTreeline Fluctuations, Sweden

Dahl and Nesje 1996

Page 26: Quaternary Environments Non-Marine Biological Evidence.

Vegetation Zones with ElevationVegetation Zones with Elevation

Page 27: Quaternary Environments Non-Marine Biological Evidence.

Vegetation Zones with ElevationVegetation Zones with Elevation

Page 28: Quaternary Environments Non-Marine Biological Evidence.

Changes in Major Vegetation Zones for Changes in Major Vegetation Zones for 22,000 years in Nevada22,000 years in Nevada

Page 29: Quaternary Environments Non-Marine Biological Evidence.

Packrats (Neotoma)Packrats (Neotoma)

First used in Quaternary Paleoecology First used in Quaternary Paleoecology introduced by introduced by Phillip WellsPhillip Wells (Wells and (Wells and Jorgensen, 1964), a zoologist doing vegetation Jorgensen, 1964), a zoologist doing vegetation reconnaissance on the Nevada Test Site.reconnaissance on the Nevada Test Site.

Collect all vegetation around the middenCollect all vegetation around the midden Preserved by amberat (urine)Preserved by amberat (urine) Also bring in pollenAlso bring in pollen

Page 30: Quaternary Environments Non-Marine Biological Evidence.

Packrat Midden Packrat Midden LocationsLocations

Page 31: Quaternary Environments Non-Marine Biological Evidence.

Davis: http://www.geo.arizona.edu/palynology/geos462/28packrats.html

Page 32: Quaternary Environments Non-Marine Biological Evidence.

Packrat MiddenPackrat Midden

Page 33: Quaternary Environments Non-Marine Biological Evidence.

Packrat MiddenPackrat Midden

Page 34: Quaternary Environments Non-Marine Biological Evidence.

Packrat Midden from University of Arizona (has Giant Sloth Bones)

Page 35: Quaternary Environments Non-Marine Biological Evidence.

Macrofossils and Pollen from Packrat Macrofossils and Pollen from Packrat MiddensMiddens

Davis: http://www.geo.arizona.edu/palynology/geos462/28packrats.html

Page 36: Quaternary Environments Non-Marine Biological Evidence.

Problems with PackratsProblems with Packrats

Collected material may not represent a random Collected material may not represent a random representation of surrounding environmentrepresentation of surrounding environment

Different species have different preferencesDifferent species have different preferences Discontinuous depositsDiscontinuous deposits BioturbationBioturbation

Page 37: Quaternary Environments Non-Marine Biological Evidence.

Creosote Distribution From Packrat MiddensCreosote Distribution From Packrat Middens

Davis: http://www.geo.arizona.edu/palynology/geos462/28packrats.html

Page 38: Quaternary Environments Non-Marine Biological Evidence.

Insect StudiesInsect Studies

Organisms usedOrganisms used Coleoptera (Beetles) most commonColeoptera (Beetles) most common Diptera (Flies)Diptera (Flies) Hymenoptera (Wasps and Ants)Hymenoptera (Wasps and Ants)

Found in sedimentary deposits such as lake Found in sedimentary deposits such as lake beds or peatbeds or peat

Based on exoskeleton morphologyBased on exoskeleton morphology Little lag in assemblage changesLittle lag in assemblage changes

Page 39: Quaternary Environments Non-Marine Biological Evidence.

InsectsInsects Study of late Quaternary beetle faunas began with Study of late Quaternary beetle faunas began with

J.V. Matthews (1975) North American J.V. Matthews (1975) North American G.R. Coope's (1977) study of British deposits G.R. Coope's (1977) study of British deposits S.A. Elias (1985) western U.S.S.A. Elias (1985) western U.S.

Production Production More species of beetles than of all other animals. More species of beetles than of all other animals.

DispersalDispersal Taphonomy poorly studied, but fossils are interpreted as local, Taphonomy poorly studied, but fossils are interpreted as local,

however, many beetles can fly and their remains are present in however, many beetles can fly and their remains are present in streams.streams.

Preservation Preservation Beetle carapaces are the most resistant of all insect fossils. Their Beetle carapaces are the most resistant of all insect fossils. Their

elytrae (chitinous wing covers) are particularly abundant, heads elytrae (chitinous wing covers) are particularly abundant, heads and legs also common.and legs also common.

IdentificationIdentification Beetles are probably the best studied insect group (taxonomically), Beetles are probably the best studied insect group (taxonomically),

and their preserved remains useful in identificationand their preserved remains useful in identification

Page 40: Quaternary Environments Non-Marine Biological Evidence.

Beetle MorphologyBeetle Morphology

Page 41: Quaternary Environments Non-Marine Biological Evidence.

Reconstructed Paleotemperature Reconstructed Paleotemperature Based on Insect Remains, UKBased on Insect Remains, UK

Page 42: Quaternary Environments Non-Marine Biological Evidence.

Mutual Climate RangeMutual Climate Range

Page 43: Quaternary Environments Non-Marine Biological Evidence.

Chironomid Percentage DiagramChironomid Percentage Diagram

Page 44: Quaternary Environments Non-Marine Biological Evidence.