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Earlandite

A valid IMA mineral species - grandfathered
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About EarlanditeHide

02011870017271922587209.jpg
Arthur Earland
Formula:
Ca3[CH2(COO)-CHOH(COO)-CH2(COO)]2 · 4H2O
Colour:
White, pale yellow
Specific Gravity:
1.80 - 1.95
Crystal System:
Monoclinic
Name:
Named in honor of Arthur Earland (3 November 1866, Lewisham, London, England, UK - 27 March 1958), British oceanographer and foraminifera specialist. He studied sediments from the Weddell Sea near Antarctica returned by the ship Scotia, and identified grains of the new mineral.
Chemically identical to calcium citrate tetrahydrate - a citric acid salt.

Occurs in unconsolidated ocean floor sediment at 2,580 meters in depth.


Unique IdentifiersHide

Mindat ID:
1344
Long-form identifier:
mindat:1:1:1344:0

IMA Classification of EarlanditeHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Ca3(C6H5O7)3-2·4H2O
First published:
1936

Classification of EarlanditeHide

10.AC.10

10 : ORGANIC COMPOUNDS
A : Salts of organic acids
C : Benzine Salts
50.2.2.1

50 : ORGANIC COMPOUNDS
2 : Mellitates, Citrates, Cyanates, Acetates and Formates
31.2.1

31 : Oxalates, Citrates, Mellitates and Acetates
2 : Citrates

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
EarIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of EarlanditeHide

Transparency:
Translucent
Colour:
White, pale yellow
Comment:
Hardness not determined.
Density:
1.80 - 1.95 g/cm3 (Measured)    1.96 g/cm3 (Calculated)

Optical Data of EarlanditeHide

Type:
Biaxial (+)
RI values:
nα = 1.515 nβ = 1.530 nγ = 1.580
2V:
Measured: 60° , Calculated: 50°
Max. Birefringence:
δ = 0.065
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Moderate
Dispersion:
r > v

Chemistry of EarlanditeHide

Mindat Formula:
Ca3[CH2(COO)-CHOH(COO)-CH2(COO)]2 · 4H2O
Element Weights:
Element% weight
O50.303 %
C25.175 %
Ca21.001 %
H3.521 %

Calculated from ideal end-member formula.

Crystallography of EarlanditeHide

Crystal System:
Monoclinic
Cell Parameters:
a = 30.94 Å, b = 5.93 Å, c = 10.56 Å
β = 93.74°
Ratio:
a:b:c = 5.218 : 1 : 1.781
Unit Cell V:
1,933.36 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Veruginous, fine-grained nodules.
Comment:
Crystal System determination based on observations on synthetic material. Class and Space Group not determined.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0019542EarlanditeHerdtweck E, Kornprobst T, Sieber R, Straver L, Plank J (2011) Crystal structure, synthesis, and properties of tri-calcium di-citrate tetra-hydrate [Ca3(C6H5O7)2(H2O)2]*2H2O Zeitschrift fur Anorganische und Allgemeine Chemie 637 655-6592011synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
15.5 Å(100)
8.5 Å(4)
7.7 Å(50)
6.4 Å(4)
5.2 Å(35)
3.09 Å(6)
4.74 Å(4)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 3b: Earth’s earliest hydrosphere>4.45
17 : Marine authigenic Hadean minerals (see also #24)
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
49 : Oxic cellular biomineralization (see also #44)<0.54

Type Occurrence of EarlanditeHide

General Appearance of Type Material:
Warty,fine-grained nodules.
Place of Conservation of Type Material:
The Natural History Museum, London, England: #1936,978, 1936,979. Harvard University, Cambridge, Massachusetts, USA: #134573.U.S. National Museum of Natural History, Washington, D.C., USA: #105859, 162618.
Geological Setting of Type Material:
Unconsolidated ocean sediments.
Associated Minerals at Type Locality:

Other Language Names for EarlanditeHide

German:Earlandit
Spanish:Earlandita

Related Minerals - Strunz-mindat GroupingHide

10.AC.05MelliteAl2[C6(COO)6] · 16H2OTet. 4/mmm(4/m2/m2/m) : I41/acd
10.AC.15PigotiteAl4C6H5O10 · 13H2O (?)

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for EarlanditeHide

References for EarlanditeHide

Localities for EarlanditeHide

Showing 1 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Antarctica (TL)
 
  • West Antarctica
    • Weddell Sea
Palache et al. (1951)
 
and/or  
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