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Table 1 Results by lithology including mineralogy and texture observed in hand specimens and the texture on the calcites used for the isotopic analyses (δ13CVPDB, δ18OVPDB)

From: Preserved organic matter in a fossil Ocean Continent Transition in the Alps: the example of Totalp, SE Switzerland

Rock type

Sample number

Coordinates (UTM)

 

Locality

Macroscopic description

Mineralogical description

Texture

Carbonate texture

δ 13CVPDB (‰) Ca veins

δ 18OVPDB (‰) Ca veins

X (m)

Y (m)

Serpentinite

 Massive  serpentinite

5

561895

5188662

Parsennfurgga

Massive black serpeninite with white angular borders defining the experidotite minerals, small green chrysotile veinlets and white carbonate veinlets

Olivine completely replace by serpentine minerals, phantoms of pyroxene, magnetite, later carbonate vein; calcite veins with only one stage of crystal growing

Mesha

   

16

561522

5188399

2442 m. Obersasställi-Parsennfurga

Calcite vein, 1st generation

0.11

−10.2

 Serpentinite with numerous calcite veins

24

561514

5188009

Obersasställi

Broken serpentinite clasts from a first generation of greyish deformed calcite veins crosscut almost perpendicularly by a second generation of white calcite veins

Mainly mesh texture with rare ribbon texture; randomly dispersed anhedral magnetite grain; later veins of chrysotile

Clast supported brecciaa

Calcite vein, 1st generation

0.03

−11.75

26

561504

5188010

2442 m. Obersasställi-Parsennfurga

   

44

561518

5188415

   

47

561540

5188427

   

 Red serpentinite

71

561588

5188095

2442 m. Obersasställi-Parsennfurga

Red matrix with dark-black deformed clasts/veins with numerous calcite veins, also contain dark green serpentinite

The serpentinite is lizardite containing also talc and calcite; the red colour is due to hematite (4%)

Red serpentinite breccia

Calcite vein, 2st generation

1.37

−11.3

Serpentinite gouge

69

561929

5187152

Obersasställi

Black fine-grained deformed serpentinite with equant serpentine grain following and distributed systematicaly and fine short veinlets (chrysotile; calcite)

No thin section or XRD

Fine grained

   

 Serpentinite cataclasite

70

561929

5187152

Obersasställi

Black serpentinite with subangular serpentinie clasts showing no prefered orientation

No thin section or XRD

Fine grained

   

 Massive serpentinite*

77

561482

5187004

Weissfluhjoch

Black serpentinite with sub-rounded anhedral white-grayish peridotite mineral (pyroxene) and small chrysotile veins

No thin section or XRD

Mesh

   

78

561482

5187004

Sedimentary ophicalcite

 Limestone (Neptunian dykes)

1

561543

5188408

2442 m. Obersasställi-Parsennfurga

Fine micritic pink and red pelagic limestone; serpentine minerals as clasts and veins

Three types of carbonate crystal growing; the matrix composed of rounded to angular coarse grains with hornblend floating randomly in the matrix

Porphyro-clastica

Calcite vein, 2nd generation

1.56

−6.4

23

561514

5188009

Obersasstalli

    

 Tectono-sedimentary  ophicalcite

21

561520

5188015

Obersasställi

Red fine carbonate matrix with black anhedral serpentinite broken clasts crosscutted by calcite veins

Serpentinites clasts broken by several generation of carbonate veins; several stage of crystal growing for the carobnates;

Fine grained with clastsa

   

25

561511

5188009

Calcite vein, 1st generation

0.32

 -11.7

39

561515

5188439

2442 m. Obersasställi-Parsennfurga

Calcite vein, 1st generation

0.58

 -10.9

41

561572

5188406

Calcite vein, 2nd generation

1.78

 -7.1

42

561572

5188406

Calcite vein, 1nd and 2nd gener

0.42; 1.07

−10.3; −8.6

46

561540

5188418

   

66

564260

5190402

Near Grüenhorn

Calcite vein, undetermined generation

1.86

−6.2

 Reworked tec-sed ophicalcite

9

562586

5188578

Parsennfurga-Parsennhütte

Pink carbonate with randomly orientated elongated clast of ophicalcite (serpentinite + carbonate); numerous calcite veins

No thin section or XRD

reworkeda

   

 Vein supported serpentinite breccia

72

561929

5187152

2442 m. Obersasställi-Parsennfurga

Centimetric angular clasts of green serpentinite tectonically broken by calcite veins

No thin section or XRD

Vein supported breccia

Calcite vein, undetermined generation

1.60

−10.6

Sediments

 Radiolarite

62

564212

5190386

Near Grüenhorn from sulphide rich outcrop

Hard fine grained red siliceous rock; post deposition quartz vein perpendiulcar to the geometry of deposition

No thin section or XRD

Fine grained

Post-deposit calcite vein

−0.79

−6.4

 

68

564252

5190393

   

 Siliceous shale

60

564212

5190386

Near Grüenhorn from sulphide rich outcrop

Greyiish-reddish fine grained siliceous rock, great porosity and numerous fractures

Composed mainly by quartz (46%), plagioclase(30%), chlorite, muscovite and hematite

Fine grained

   

61

564212

5190386

   

15

564049

5189517

Gotschnagrat

Red and grey fine grained intercalated siliceous shale with deformed quartz veins

Dominated by quartz (89%) with plagioclase, muscovite, chlorite and trace of hematite

Fine grained

   

18

564213

5189544

   

 Limestone

10

562494

188558

Parsennfurga-Parsennhütte

Grey limestone with numerous calcite veins of two generation almost perpendicular to each other

Pelagic limestone, evidence of fossil organisms filled by sparry calcite

Fine grained

   

19

563790

5189694

Gotschnagrat

Calcite vein, 1st generation

0.56

−6.5

 Limestone

53

563144

5188716

South from Parsennhütte

Grey limestone with fine greyish veinlets and rare short calcite veins with pink pelagic limestone (hematite) in places

No thin section or XRD

Fine grained

   

54

563140

5188707

   

56

563140

5188707

   

57

563144

5188716

   

58

563144

5188716

   

 Carbonate (sulphide rich outcrop)

63

564212

5190386

Near Grüenhorn

Carbonate rock with deformed quartz veins; microscopic grain ofpyrite everywhere except in the quartz and calcite veins

Dominated by calcite (53%) with quartz, chlorite (12%) and pyrite

Porphyro-clastic

   

64

564212

5190386

Calcite vein, 2nd generation

1.4

−6.6

65

564252

5190393

Very fractured sample with greater porosity

   
  1. The vein generation is defined from the specific example and may not correlate across all samples
  2. * All lithology are from the lower sub-unit with the exception of the massive serpentinite (samples 77, 78)
  3. aThin section of the lithology is observed