Table 1 Semi-quantitative distribution of sulfide minerals and main element compositions of hydrothermal precipitates from the Kairei and Pelagia hydrothermal vent fields.

From: Hydrothermal chimneys host habitat-specific microbial communities: analogues for studying the possible impact of mining seafloor massive sulfide deposits

Sample

 

Semi-quantitative mineral composition

Quantitative main element composition

Description

Kairei area

INDEX2016-06ROV03-A

S1

ccp+++

py/mrc+

sp++

Cu: 12.6–25.8 wt.%

Fe: 18.5–25.6 wt.%

Zn: 10.3–29.7 wt.%

fragment of inactive chimney,

Kairei active zone

INDEX2016-06ROV03-N

S2

ccp 0

py/mrc+++

sp+++

iso 0

Cu: 0.3–0.4 wt.%

Fe: 23.8–28.3 wt.%

Zn: 28.9–31.7 wt.%

inactive beehive shaped chimney,

Kairei inactive zone

INDEX2016-12ROV06-E

S7

ccp +++

py/mrc+

sp++

Cu: 18.1–26.2 wt.%

Fe: 21.2–28.4 wt.%

Zn: 6.8–24.3 wt.%

inactive chimney edifice,

Kairei active zone

INDEX2016-12ROV06-F

S8

ccp+++

py/mrc+

sp++

anh 0

Cu: 25.3–26.5 wt.%

Fe: 27.1–29.0 wt.%

Zn: 6.5–10.7 wt.%

fragment of active chimney,

Kairei HF

Pelagia area

INDEX2016-16ROV08-E

S5

ccp+

py/mrc+++

sp +

Cu: 1.3–7.4 wt.%

Fe: 33.3–44.4 wt.%

Zn: 0.9–12.2 wt.%

active beehive shaped chimney,

Pelagia HF

INDEX2016-20ROV10-G

S6

ccp 0

py/mrc+++

po+

sp++

iso +

Cu: 1.5–1.7 wt.%

Fe: 41.5–42.2 wt.%

Zn: 7.0–7.1 wt.%

fragment of active chimney,

Pelagia HF

INDEX2016-20ROV10-J

S4

ccp 0

py/mrc+++

sp+

Cu: 0.1–0.8 wt.%

Fe: 29.9–36.2 wt.%

Zn: 0.5–3.3 wt.%

fragment of beehive shaped inactive chimney,

Pelagia HF

  1. Geochemical compositions are given in min.-max. values from interior to outer part of the sample. Mineral abbreviations: ccp = chalcoyprite (CuFeS2), py/mrc = pyrite/marcasite (FeS2), sp = sphalerite (ZnS), po = pyrrhotite (Fe1−xS), iso = isocubanite (CuFe2S3), anh = anhydrite (CaSO4) +++ abundant, ++ common, + traces, 0 acessory. HF = hydrothermal field.