1
Rachel Grandpre 1 , Elisabeth Sikes 2 , Samantha Burgess 3 , Thomas Guilderson 4 1 Smith College, Northampton, MA; 2 Rutgers University, Institute of Marine and Coastal Sciences, New Brunswick, NJ; 3 University of Auckland, School of Environmental and Marine Sciences, Auckland, New Zealand, 4 Lawrence Livermore National Laboratory, Center for Accelerator Mass Spectrometry, Livermore, CA Figure 1: Figure 1: The 14 C system as described above. Figure 2: Figure 2: This solitary deep water coral, Goniocorella dumosa, was sampled from the South Chatham Rise at 395m. The The 14 14 C Ocean System C Ocean System The formation of 14 C takes place in the atmosphere and is then incorporated into CO 2 , which is transferred to the ocean by gas exchange at the surface. Water located above the thermocline maintains a constant age because of the continuous input of new radiocarbon. Water below the thermocline is cut off from the atmosphere and begins the aging process as 14 C decays. Via global thermohaline circulation, water travels below the thermocline and ages as it travels. The vertical distributions of radiocarbon in the ocean can be used to show patterns of ocean circulation and horizontal movement. The results of this study will provide a more accurate picture of the circulation in New Zealand Currently only general knowledge exists regarding the circulation of deep water in the New Zealand area. In the past it has been assumed that the ages of New Zealand waters match with what has been observed regionally in the South Pacific. By determining radiocarbon ages of modern deep water corals of varying depths, the specific data regarding the area around New Zealand will be better understood. Why Deep Corals? Why Deep Corals? The radiocarbon ages of the carbonate that makes up the coral skeleton will provide ages that are the same as that of the water mass in which the corals grow. The corals were alive when acquired, and therefore indicate the age of the water at the time of sampling. By having corals from a range of depths, modern age estimates can be made for multiple areas of the water column. Study Area – New Zealand Study Area – New Zealand W O C E Station 182,B ay ofPlenty,and 3 K ings C 14 A ge vs.D epth 0 200 400 600 800 1000 1200 1400 1600 0 200 400 600 800 1000 1200 1400 1600 1800 C onventionalC 14 Age (yrs B P) D epth (m ) W O C E 182 (32.5 S ) 3 K ings B ay ofP lenty D eep C oralC 14 Age vs.D epth (Excluding BountyP lateau D ata ) 0 200 400 600 800 1000 1200 1400 0 200 400 600 800 1000 1200 1400 C onventionalC 14 Age (yrs B P) Depth (m ) 3 K ings Bayof P lenty N orth C hatham Rise South C hatham Rise W est C oast of S outh Island Auckland Islands Figure 5: Figure 5: The 14 C ages of our corals plotted against the depth of sampling. Not included is one sample assumed to be dead upon sampling because the radiocarbon age was 6830 14 C yr BP. Figure 6: Figure 6: Our 14 C data from 2 regions plotted with WOCE sta. 182 data. The 3 Kings ages match up with the WOCE data indicating the expected trends at similar depths. The Bay of Plenty ages are much older at shallower depths. There are several possible explanations There are several possible explanations for the old shallow water at this location: for the old shallow water at this location: (listed in decreasing order of (listed in decreasing order of plausibility) plausibility) The water travels a different path The water travels a different path through the ocean and ages below the through the ocean and ages below the thermocline for and extended amount of thermocline for and extended amount of time. time. There may be a “basin effect” in the Bay There may be a “basin effect” in the Bay of Plenty, and there is limited circulation of Plenty, and there is limited circulation causing local aging. causing local aging. The Chatham Rise The Chatham Rise Figure 7: Figure 7: In this location, significant turbulence due to strong currents associated with the subtropical front (STF) and the shallow bathymetric profile formed by the Chatham Rise cause water from the surface to mix down. This brings modern carbon to deep modern carbon to deep depths depths. Figure 4: Figure 4: This figure illustrates how bomb radiocarbon (any 14 C value above zero) penetrates below the thermocline. The thermocline in the plot is at about 200m and we see bomb radiocarbon as deep as 600m. Special thanks to Naomi Fleming (IMCS) and Jennifer Bosch (IMCS) for assistance with the Mat Lab plots, and to Dr. James Wright (Geology Dept. Rutgers) for running the stable isotope data. Funding for analyses run in Australia came from ANSTO grant 01/69 (to ELS) and for samples run at LLNL from NSF OCE0136651 (to ELS). By obtaining the radiocarbon ages of living deep water corals from various locations around New Zealand, we now have a more detailed view of the local circulation of water masses. The 14 C ages of the corals from many locations match with WOCE data indicating that circulation is what was expected regionally. Other locations show old water at shallow depths. This is most likely because the water taking an alternate path around the ocean and has the opportunity to get older. At the Chatham Rise there are very modern ages for the water at greater depths due to turbulent mixing associated with the STF and the bathymetric high. D epth (m ) Latitude C hatham Rise -99 171 -3 -84 24 11 22 R 333 R 332 R 327 R 326 R 324 R 312 47 S 46 S 45 S 44 S 43 S 42 S 41 S 1000 900 800 700 600 500 400 300 200 100 0 14 C ( o /oo) -100 -50 0 50 100 150 200 165 E 170 E 175 E 180 E 175 W 170 W 50 S 45 S 40 S 35 S Z9025 Z9226 Z8919 Z9618 I721 I676 E800 Z9953 X 487 Z9792 Z9581 Z9364 T8 N ew Zealand N orth Island S outh Island C hatham R ise B ounty P lateau A uckland Islands Three K ings B ay ofP lenty Figure 3: Figure 3: Map of New Zealand including sample locations.

Rachel Grandpre 1 , Elisabeth Sikes 2 , Samantha Burgess 3 , Thomas Guilderson 4

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Assessing New Zealand Deep Water Ages Using Radiocarbon Dating of Deep Corals. Rachel Grandpre 1 , Elisabeth Sikes 2 , Samantha Burgess 3 , Thomas Guilderson 4 - PowerPoint PPT Presentation

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  • Rachel Grandpre1, Elisabeth Sikes2, Samantha Burgess3, Thomas Guilderson41Smith College, Northampton, MA; 2Rutgers University, Institute of Marine and Coastal Sciences, New Brunswick, NJ; 3University of Auckland, School of Environmental and Marine Sciences, Auckland, New Zealand, 4Lawrence Livermore National Laboratory, Center for Accelerator Mass Spectrometry, Livermore, CAFigure 1: The 14C system as described above.Figure 2: This solitary deep water coral, Goniocorella dumosa, was sampled from the South Chatham Rise at 395m.The 14C Ocean System

    The formation of 14C takes place in the atmosphere and is then incorporated into CO2, which is transferred to the ocean by gas exchange at the surface. Water located above the thermocline maintains a constant age because of the continuous input of new radiocarbon. Water below the thermocline is cut off from the atmosphere and begins the aging process as 14C decays. Via global thermohaline circulation, water travels below the thermocline and ages as it travels. The vertical distributions of radiocarbon in the ocean can be used to show patterns of ocean circulation and horizontal movement. The results of this study will provide a more accurate picture of the circulation in New Zealand waters. Currently only general knowledge exists regarding the circulation of deep water in the New Zealand area. In the past it has been assumed that the ages of New Zealand waters match with what has been observed regionally in the South Pacific. By determining radiocarbon ages of modern deep water corals of varying depths, the specific data regarding the area around New Zealand will be better understood. Why Deep Corals?

    The radiocarbon ages of the carbonate that makes up the coral skeleton will provide ages that are the same as that of the water mass in which the corals grow. The corals were alive when acquired, and therefore indicate the age of the water at the time of sampling. By having corals from a range of depths, modern age estimates can be made for multiple areas of the water column. Study Area New Zealand

    Figure 5: The 14C ages of our corals plotted against the depth of sampling. Not included is one sample assumed to be dead upon sampling because the radiocarbon age was 6830 14C yr BP.

    Figure 6: Our 14C data from 2 regions plotted with WOCE sta. 182 data. The 3 Kings ages match up with the WOCE data indicating the expected trends at similar depths. The Bay of Plenty ages are much older at shallower depths. There are several possible explanations for the old shallow water at this location: (listed in decreasing order of plausibility)The water travels a different path through the ocean and ages below the thermocline for and extended amount of time.There may be a basin effect in the Bay of Plenty, and there is limited circulation causing local aging.There could be a local source of dead carbon from a deep sea vent or outgassing of CO2 from volcanoes.The Chatham RiseFigure 7: In this location, significant turbulence due to strong currents associated with the subtropical front (STF) and the shallow bathymetric profile formed by the Chatham Rise cause water from the surface to mix down. This brings modern carbon to deep depths. Figure 4:This figure illustrates how bomb radiocarbon (any 14C value above zero) penetrates below the thermocline. The thermocline in the plot is at about 200m and we see bomb radiocarbon as deep as 600m.Special thanks to Naomi Fleming (IMCS) and Jennifer Bosch (IMCS) for assistance with the Mat Lab plots, and to Dr. James Wright (Geology Dept. Rutgers) for running the stable isotope data. Funding for analyses run in Australia came from ANSTO grant 01/69 (to ELS) and for samples run at LLNL from NSF OCE0136651 (to ELS).By obtaining the radiocarbon ages of living deep water corals from various locations around New Zealand, we now have a more detailed view of the local circulation of water masses.

    The 14C ages of the corals from many locations match with WOCE data indicating that circulation is what was expected regionally.Other locations show old water at shallow depths. This is most likely because the water taking an alternate path around the ocean and has the opportunity to get older.At the Chatham Rise there are very modern ages for the water at greater depths due to turbulent mixing associated with the STF and the bathymetric high.Figure 3: Map of New Zealand including sample locations.

  • sample list 2004

    Deep Coral Samplesgreen=new samplesblue =duplicates of 2001 samples

    red = duplicates of new samples*** = labeled incorrectly on vial as Z9272

    Station #LocationLatitudeLongitudeDepthd13Cfraction modern?14C14C ageCAMS #Species

    Z9953South Chatham Rise Crest43.66-179.77370m41.02240.003915.73.9Modern107183Goniocorella dumosa

    Z9953 #2South Chatham Rise Crest43.66-179.77370mGoniocorella dumosa

    I676Bounty Plateau48.16-179.33817mSolenosmilla variabilis

    E800West coast of the South Island45.34166.69~700mSolenosmilla variabilis

    Z90263 Kings31.97174.26~ 700mEnallopsammia rostrata

    Z9025 #23 Kings31.97174.26~1200m40.85950.0033-146.13.3121535107184Enallopsammia rostrata

    X487North Chatham Rise42.70-179.67~820m40.90070.0034-105.23.484035Madrepora oculata

    Z8919 # 2Bay of Plenty36.50176.511000m40.86120.0034-144.43.4120035107186Enallopsammia rostrata

    Z9581Auckland Islands50.04165.95850mEnallopsammia rostrata

    Z9226 #2Bay of Plenty37.12177.29600mEnallopsammia rostrata

    Z9364Auckland Islands50.07165.911000mEnallopsammia rostrata

    Z9792***North Chatham Rise42.76-179.90~940m41.17130.0047163.74.7>Modern107187Madrepora oculata

    X484North Chatham Rise42.76-179.90~980m40.89490.0046-110.94.689045107188Madrepora oculata

    X484 #2North Chatham Rise42.76-179.90~980mMadrepora oculata

    T8South Chatham Rise44.32176.24492m40.91630.0035-89.73.570035107189Goniocorella dumosa

    T8 #2South Chatham Rise44.32176.24492mGoniocorella dumosa

    I721South Chatham Rise Crest44.12175.77540m40.99690.0038-9.63.8Modern107190Goniocorella dumosa

    Z9618South Chatham Rise Crest43.36178.95395mGoniocorella dumosa

    Sample List 2001

    Deep Coral Samples 2001

    Station #LocationLatitudeLongitudeDepth of Sample14C ageerror yrs 1sigma% modern carbonerror 1sigANSTO codeSpecies

    Z90263 Kings31.97174.26~ 700m453099.420.37OZF318Enallopsammia rostrata

    Z90253 Kings31.97174.26~1200m11204086.980.40OZF317Enallopsammia rostrata

    Z9226Bay of Plenty37.12177.29600m8153590.360.35OZF319Enallopsammia rostrata

    Z8919Bay of Plenty36.50176.511000m11404086.730.36OZF316Enallopsammia rostrata

    X487North Chatham Rise42.70-179.67~820m8403590.060.37OZF315Madrepora oculata

    Z9792North Chatham Rise42.76-179.90~940mmodernn/a145.500.53OZF320Madrepora oculata

    Z9618South Chatham Rise Crest43.36178.95395mmodernn/a102.790.40OZF323Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.77540 mmodernn/a101.230.40OZF314Goniocorella dumosa

    I676Bounty Plateau48.16-179.33817m68305042.710.22OZF313Solenosmilla variabilis

    E800West coast of the South Island45.34166.69~700m11304086.870.36OZF312Solenosmilla variabilis

    Z9581Auckland Islands50.04165.95850m3153596.150.38OZF322Enallopsammia rostrata

    Z9364Auckland Islands50.07165.911000m9153589.260.35OZF321Enallopsammia rostrata

    14C results 2001+2004

    Deep Coral SamplesBlack = 2001

    Red = 2004

    20012004

    Station #LocationLatitudeLongitudeDepth (m)14C ageerror yrs 1sigmafraction Modern% modern carbonerror 1sigAMS #CAMS #Species

    Z90263 Kings31.97174.26~700m45300.994299.420.37OZF318Enallopsammia rostrata

    Z90253 Kings31.97174.26~1200m1120400.869886.980.40OZF317Enallopsammia rostrata

    Z9025 #23 Kings31.97174.26~1200m1215350.859585.950.0033107184Enallopsammia rostrata

    Z9226Bay of Plenty37.12177.29600m815350.903690.360.35OZF319Enallopsammia rostrata

    Z8919Bay of Plenty36.50176.511000m1140400.867386.730.36OZF316Enallopsammia rostrata

    Z8919 # 2Bay of Plenty36.50176.511000m1200350.861286.120.0034107186Enallopsammia rostrata

    X487North Chatham Rise42.70-179.67~820m840350.900690.060.37OZF315Madrepora oculata

    X487North Chatham Rise42.7-179.67~820m840350.900790.070.0034107185Madrepora oculata

    Z9792***North Chatham Rise42.76-179.90~940mmodernn/a1.4550145.500.53OZF320Madrepora oculata

    Z9792***North Chatham Rise42.76-179.90~940m>modernn/a1.1713117.130.0047107187Madrepora oculata

    Z9618South Chatham Rise Crest43.36178.95395mmodernn/a1.0279102.790.40OZF323Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.77540mmodernn/a1.0123101.230.40OZF314Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.77540mmodernn/a0.996999.690.0038107190Goniocorella dumosa

    I676Bounty Plateau,48.16-179.33817m6830500.427142.710.22OZF313Solenosmilla variabilis

    E800West coast of the South Island45.34166.69~700m1130400.868786.870.36OZF312Solenosmilla variabilis

    Z9581Auckland Islands50.04165.95850m315350.961596.150.38OZF322Enallopsammia rostrata

    Z9364Auckland Islands50.07165.911000m915350.892689.260.35OZF321Enallopsammia rostrata

    Z9953South Chatham Rise Crest43.66-179.77370mmodernn/a1.0224102.240.0039107183Goniocorella dumosa

    X484North Chatham Rise42.76-179.90~980mmodernn/a0.996999.690.0038107190Goniocorella dumosa

    T8South Chatham Rise44.32176.24492m700350.916391.630.0035107189Goniocorella dumosa

    14C results (chart ready)

    Deep Coral SamplesBlack = 2001

    Red = 2004

    error yrspercent20012004

    Station #LocationLatitudeLongitudeDepth (m)14C num age14C age14 age w/ mod1sigmafraction ModernD14C (o/oo)modern carbonerror 1sigAMS #CAMS #Species

    Z90263 Kings31.97174.26700454547300.9942-5.800099.420.37OZF318Enallopsammia rostrata

    Z90253 Kings31.97174.261200112011201121400.8698-130.200086.980.40OZF317Enallopsammia rostrata

    Z9025 #23 Kings31.97174.261200121512151217350.8595-140.530485.950.0033107184Enallopsammia rostrata

    Z9226Bay of Plenty37.12177.29600815815814350.9036-96.400090.360.35OZF319Enallopsammia rostrata

    Z8919Bay of Plenty36.50176.511000114011401144400.8673-132.700086.730.36OZF316Enallopsammia rostrata

    Z8919 # 2Bay of Plenty36.50176.511000120012001201350.8612-138.827186.120.0034107186Enallopsammia rostrata

    X487North Chatham Rise42.70-179.67820840840841350.9006-99.400090.060.37OZF315Madrepora oculata

    X487North Chatham Rise42.7-179.67820840840840350.9007-99.292690.070.0034107185Madrepora oculata

    Z9792North Chatham Rise42.76-179.909400modern-3012n/a1.4550455.0000145.500.53OZF320Madrepora oculata

    Z9792North Chatham Rise42.76-179.909400>modern-1270n/a1.1713171.3120117.130.0047107187Madrepora oculata

    X484North Chatham Rise42.76-179.909800modern25n/a0.9969-3.106299.690.0038107190Goniocorella dumosa

    T8South Chatham Rise44.32176.24492700700702350.9163-83.691991.630.0035107189Goniocorella dumosa

    Z9618South Chatham Rise Crest43.36178.953950modern-221n/a1.027927.9000102.790.40OZF323Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.775400modern-98n/a1.012312.3000101.230.40OZF314Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.775400modern25n/a0.9969-3.106299.690.0038107190Goniocorella dumosa

    Z9953South Chatham Rise Crest43.66-179.773700modern-178n/a1.022422.4037102.240.0039107183Goniocorella dumosa

    I676Bounty Plateau48.16-179.33817683068306834500.4271-572.900042.710.22OZF313Solenosmilla variabilis

    E800West coast of the South Island45.34166.69700113011301131400.8687-131.300086.870.36OZF312Solenosmilla variabilis

    Z9581Auckland Islands50.04165.95850315315315350.9615-38.500096.150.38OZF322Enallopsammia rostrata

    Z9364Auckland Islands50.07165.911000915915913350.8926-107.400089.260.35OZF321Enallopsammia rostrata

    age depth plot

    700

    1200

    1200

    600

    1000

    1000

    820

    820

    940

    940

    980

    492

    395

    540

    540

    370

    817

    700

    850

    1000

    Coral 14C ages vs. Depth

    Conventional C14 Age

    Depth (m)

    Deep Coral C14 Ages vs. Depth

    age depth w locations

    700600820492817700850

    120010008203951000

    12001000940540

    940540

    980370

    3 Kings

    Bay of Plenty

    North Chatham Rise

    South Chatham Rise

    Bounty Plateau

    West Coast of South Island

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    Deep Coral C14 Age vs. Depth

    age depth (no Bounty Plat)

    700600820492700850

    120010008203951000

    12001000940540

    940540

    980370

    3 Kings

    Bay of Plenty

    North Chatham Rise

    South Chatham Rise

    West Coast of South Island

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    Deep Coral C14 Age vs. Depth(Excluding Bounty Plateau Data )

    age depth no Bounty or chatham

    700600700850

    120010001000

    12001000

    3 Kings

    Bay of Plenty

    West Coast of South Island

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    Deep Coral C14 Age vs. Depth(Excluding Bounty Plateau and Chatham Rise Data)

    Sta14 vs Our C14 ages

    70054.6

    120094.3

    1200159.7

    600209

    1000258.2

    1000308.7

    820359

    820433.5

    940508.2

    940608.6

    980709.7

    492808.3

    395907.5

    5401007.7

    5401107.8

    3701257.5

    8171408.5

    7001609.9

    8501811.2

    10002012

    2214.4

    2418.3

    2619.2

    2823.6

    Deep Coral Samples

    WOCE 14 (42.995 S)

    Conventional C14 Age

    Depth (m)

    WOCE Station 14 and Deep Corals C14 Age vs. Depth

    Sta14 vs Our C14 ages no bount

    70054.6

    120094.3

    1200159.7

    600209

    1000258.2

    1000308.7

    820359

    820433.5

    940508.2

    940608.6

    980709.7

    492808.3

    395907.5

    5401007.7

    5401107.8

    3701257.5

    7001408.5

    8501609.9

    10001811.2

    2012

    2214.4

    2418.3

    2619.2

    2823.6

    C14 Age of Coral Samples

    WOCE 14 (42.995 S)

    Conventional C14 Age

    Depth (m)

    WOCE Station 14 and Deep CoralsC14 Age vs. Depth(Excluding Bounty Plateau Data)

    Sta 14 and Locations

    54.6700600820492700850

    94.3120010008203951000

    159.712001000940540

    209940540

    258.2980370

    308.7

    359

    433.5

    508.2

    608.6

    709.7

    808.3

    907.5

    1007.7

    1107.8

    1257.5

    1408.5

    1609.9

    1811.2

    2012

    2214.4

    2418.3

    2619.2

    2823.6

    WOCE 14 (42.995 S)

    3 Kings

    Bay of Plenty

    North Chatham Rise

    South Chatham Rise

    West Coast of South Island

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    WOCE Station 14 and Deep Coral C14 Age vs. Depth

    sta182 vs 3kings

    17.7700

    128.21200

    207.71200

    306.8

    356.9

    406.5

    506.3

    606.7

    707.2

    807.5

    906.2

    1002.3

    1100.6

    1297.5

    1395

    1492.1

    WOCE 182 (32.5 S)

    3 Kings

    Conventional C14 Age

    Depth (m)

    WOCE Station 183 and 3 Kings C14 Age vs. Depth

    Sta 182 and BayOPlen

    17.7700600

    128.212001000

    207.712001000

    306.8

    356.9

    406.5

    506.3

    606.7

    707.2

    807.5

    906.2

    1002.3

    1100.6

    1297.5

    1395

    1492.1

    WOCE 182 (32.5 S)

    3 Kings

    Bay of Plenty

    Conventional C14 Age (yrs BP)

    Depth (m)

    WOCE Station 182, Bay of Plenty, and 3 Kings C14 Age vs. Depth

    Sta22 and Auckland

    601.9850

    699.21000

    802.5

    904

    1005.1

    1209.6

    1412.7

    1616.3

    1815.9

    2011.3

    2203.7

    2404.6

    2607.2

    3004.3

    3209.9

    3409.8

    3614.2

    WOCE 22 (47 S)

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    WOCE Station 22 and Auckland Islands C14 Age vs. Depth

    N. Chat and R332

    8200

    82030

    94060

    940100

    980200

    300

    400

    500

    600

    800

    1000

    North Chatham Rise

    R332

    Conventional C14 Age

    Depth (m)

    R332 (42o S, 179o E) and North Chatham RiseC14 Age vs. Depth

    S Chat and R324

    49220

    39550

    540100

    540200

    370400

    600

    800

    1000

    South Chatham Rise

    R324

    Conventional C14 Age

    Depth (m)

    R324 (44o59.9 S, 179o E) and South Chatham RiseC14 Age vs Depth

    Sheet2

    Sheet3

    sample list 2004

    Deep Coral Samplesgreen=new samplesblue =duplicates of 2001 samples

    red = duplicates of new samples*** = labeled incorrectly on vial as Z9272

    Station #LocationLatitudeLongitudeDepthd13Cfraction modern?14C14C ageCAMS #Species

    Z9953South Chatham Rise Crest43.66-179.77370m41.02240.003915.73.9Modern107183Goniocorella dumosa

    Z9953 #2South Chatham Rise Crest43.66-179.77370mGoniocorella dumosa

    I676Bounty Plateau48.16-179.33817mSolenosmilla variabilis

    E800West coast of the South Island45.34166.69~700mSolenosmilla variabilis

    Z90263 Kings31.97174.26~ 700mEnallopsammia rostrata

    Z9025 #23 Kings31.97174.26~1200m40.85950.0033-146.13.3121535107184Enallopsammia rostrata

    X487North Chatham Rise42.70-179.67~820m40.90070.0034-105.23.484035Madrepora oculata

    Z8919 # 2Bay of Plenty36.50176.511000m40.86120.0034-144.43.4120035107186Enallopsammia rostrata

    Z9581Auckland Islands50.04165.95850mEnallopsammia rostrata

    Z9226 #2Bay of Plenty37.12177.29600mEnallopsammia rostrata

    Z9364Auckland Islands50.07165.911000mEnallopsammia rostrata

    Z9792***North Chatham Rise42.76-179.90~940m41.17130.0047163.74.7>Modern107187Madrepora oculata

    X484North Chatham Rise42.76-179.90~980m40.89490.0046-110.94.689045107188Madrepora oculata

    X484 #2North Chatham Rise42.76-179.90~980mMadrepora oculata

    T8South Chatham Rise44.32176.24492m40.91630.0035-89.73.570035107189Goniocorella dumosa

    T8 #2South Chatham Rise44.32176.24492mGoniocorella dumosa

    I721South Chatham Rise Crest44.12175.77540m40.99690.0038-9.63.8Modern107190Goniocorella dumosa

    Z9618South Chatham Rise Crest43.36178.95395mGoniocorella dumosa

    Sample List 2001

    Deep Coral Samples 2001

    Station #LocationLatitudeLongitudeDepth of Sample14C ageerror yrs 1sigma% modern carbonerror 1sigANSTO codeSpecies

    Z90263 Kings31.97174.26~ 700m453099.420.37OZF318Enallopsammia rostrata

    Z90253 Kings31.97174.26~1200m11204086.980.40OZF317Enallopsammia rostrata

    Z9226Bay of Plenty37.12177.29600m8153590.360.35OZF319Enallopsammia rostrata

    Z8919Bay of Plenty36.50176.511000m11404086.730.36OZF316Enallopsammia rostrata

    X487North Chatham Rise42.70-179.67~820m8403590.060.37OZF315Madrepora oculata

    Z9792North Chatham Rise42.76-179.90~940mmodernn/a145.500.53OZF320Madrepora oculata

    Z9618South Chatham Rise Crest43.36178.95395mmodernn/a102.790.40OZF323Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.77540 mmodernn/a101.230.40OZF314Goniocorella dumosa

    I676Bounty Plateau48.16-179.33817m68305042.710.22OZF313Solenosmilla variabilis

    E800West coast of the South Island45.34166.69~700m11304086.870.36OZF312Solenosmilla variabilis

    Z9581Auckland Islands50.04165.95850m3153596.150.38OZF322Enallopsammia rostrata

    Z9364Auckland Islands50.07165.911000m9153589.260.35OZF321Enallopsammia rostrata

    14C results 2001+2004

    Deep Coral SamplesBlack = 2001

    Red = 2004

    20012004

    Station #LocationLatitudeLongitudeDepth (m)14C ageerror yrs 1sigmafraction Modern% modern carbonerror 1sigAMS #CAMS #Species

    Z90263 Kings31.97174.26~700m45300.994299.420.37OZF318Enallopsammia rostrata

    Z90253 Kings31.97174.26~1200m1120400.869886.980.40OZF317Enallopsammia rostrata

    Z9025 #23 Kings31.97174.26~1200m1215350.859585.950.0033107184Enallopsammia rostrata

    Z9226Bay of Plenty37.12177.29600m815350.903690.360.35OZF319Enallopsammia rostrata

    Z8919Bay of Plenty36.50176.511000m1140400.867386.730.36OZF316Enallopsammia rostrata

    Z8919 # 2Bay of Plenty36.50176.511000m1200350.861286.120.0034107186Enallopsammia rostrata

    X487North Chatham Rise42.70-179.67~820m840350.900690.060.37OZF315Madrepora oculata

    X487North Chatham Rise42.7-179.67~820m840350.900790.070.0034107185Madrepora oculata

    Z9792***North Chatham Rise42.76-179.90~940mmodernn/a1.4550145.500.53OZF320Madrepora oculata

    Z9792***North Chatham Rise42.76-179.90~940m>modernn/a1.1713117.130.0047107187Madrepora oculata

    Z9618South Chatham Rise Crest43.36178.95395mmodernn/a1.0279102.790.40OZF323Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.77540mmodernn/a1.0123101.230.40OZF314Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.77540mmodernn/a0.996999.690.0038107190Goniocorella dumosa

    I676Bounty Plateau,48.16-179.33817m6830500.427142.710.22OZF313Solenosmilla variabilis

    E800West coast of the South Island45.34166.69~700m1130400.868786.870.36OZF312Solenosmilla variabilis

    Z9581Auckland Islands50.04165.95850m315350.961596.150.38OZF322Enallopsammia rostrata

    Z9364Auckland Islands50.07165.911000m915350.892689.260.35OZF321Enallopsammia rostrata

    Z9953South Chatham Rise Crest43.66-179.77370mmodernn/a1.0224102.240.0039107183Goniocorella dumosa

    X484North Chatham Rise42.76-179.90~980mmodernn/a0.996999.690.0038107190Goniocorella dumosa

    T8South Chatham Rise44.32176.24492m700350.916391.630.0035107189Goniocorella dumosa

    14C results (chart ready)

    Deep Coral SamplesBlack = 2001

    Red = 2004

    error yrspercent20012004

    Station #LocationLatitudeLongitudeDepth (m)14C num age14C age14 age w/ mod1sigmafraction ModernD14C (o/oo)modern carbonerror 1sigAMS #CAMS #Species

    Z90263 Kings31.97174.26700454547300.9942-5.800099.420.37OZF318Enallopsammia rostrata

    Z90253 Kings31.97174.261200112011201121400.8698-130.200086.980.40OZF317Enallopsammia rostrata

    Z9025 #23 Kings31.97174.261200121512151217350.8595-140.530485.950.0033107184Enallopsammia rostrata

    Z9226Bay of Plenty37.12177.29600815815814350.9036-96.400090.360.35OZF319Enallopsammia rostrata

    Z8919Bay of Plenty36.50176.511000114011401144400.8673-132.700086.730.36OZF316Enallopsammia rostrata

    Z8919 # 2Bay of Plenty36.50176.511000120012001201350.8612-138.827186.120.0034107186Enallopsammia rostrata

    X487North Chatham Rise42.70-179.67820840840841350.9006-99.400090.060.37OZF315Madrepora oculata

    X487North Chatham Rise42.7-179.67820840840840350.9007-99.292690.070.0034107185Madrepora oculata

    Z9792North Chatham Rise42.76-179.909400modern-3012n/a1.4550455.0000145.500.53OZF320Madrepora oculata

    Z9792North Chatham Rise42.76-179.909400>modern-1270n/a1.1713171.3120117.130.0047107187Madrepora oculata

    X484North Chatham Rise42.76-179.909800modern25n/a0.9969-3.106299.690.0038107190Goniocorella dumosa

    T8South Chatham Rise44.32176.24492700700702350.9163-83.691991.630.0035107189Goniocorella dumosa

    Z9618South Chatham Rise Crest43.36178.953950modern-221n/a1.027927.9000102.790.40OZF323Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.775400modern-98n/a1.012312.3000101.230.40OZF314Goniocorella dumosa

    I721South Chatham Rise Crest44.12175.775400modern25n/a0.9969-3.106299.690.0038107190Goniocorella dumosa

    Z9953South Chatham Rise Crest43.66-179.773700modern-178n/a1.022422.4037102.240.0039107183Goniocorella dumosa

    I676Bounty Plateau48.16-179.33817683068306834500.4271-572.900042.710.22OZF313Solenosmilla variabilis

    E800West coast of the South Island45.34166.69700113011301131400.8687-131.300086.870.36OZF312Solenosmilla variabilis

    Z9581Auckland Islands50.04165.95850315315315350.9615-38.500096.150.38OZF322Enallopsammia rostrata

    Z9364Auckland Islands50.07165.911000915915913350.8926-107.400089.260.35OZF321Enallopsammia rostrata

    age depth plot

    700

    1200

    1200

    600

    1000

    1000

    820

    820

    940

    940

    980

    492

    395

    540

    540

    370

    817

    700

    850

    1000

    Coral 14C ages vs. Depth

    Conventional C14 Age

    Depth (m)

    Deep Coral C14 Ages vs. Depth

    age depth w locations

    700600820492817700850

    120010008203951000

    12001000940540

    940540

    980370

    3 Kings

    Bay of Plenty

    North Chatham Rise

    South Chatham Rise

    Bounty Plateau

    West Coast of South Island

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    Deep Coral C14 Age vs. Depth

    age depth (no Bounty Plat)

    700600820492700850

    120010008203951000

    12001000940540

    940540

    980370

    3 Kings

    Bay of Plenty

    North Chatham Rise

    South Chatham Rise

    West Coast of South Island

    Auckland Islands

    Conventional C14 Age (yrs BP)

    Depth (m)

    Deep Coral C14 Age vs. Depth(Excluding Bounty Plateau Data )

    age depth no Bounty or chatham

    700600700850

    120010001000

    12001000

    3 Kings

    Bay of Plenty

    West Coast of South Island

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    Deep Coral C14 Age vs. Depth(Excluding Bounty Plateau and Chatham Rise Data)

    Sta14 vs Our C14 ages

    70054.6

    120094.3

    1200159.7

    600209

    1000258.2

    1000308.7

    820359

    820433.5

    940508.2

    940608.6

    980709.7

    492808.3

    395907.5

    5401007.7

    5401107.8

    3701257.5

    8171408.5

    7001609.9

    8501811.2

    10002012

    2214.4

    2418.3

    2619.2

    2823.6

    Deep Coral Samples

    WOCE 14 (42.995 S)

    Conventional C14 Age

    Depth (m)

    WOCE Station 14 and Deep Corals C14 Age vs. Depth

    Sta14 vs Our C14 ages no bount

    70054.6

    120094.3

    1200159.7

    600209

    1000258.2

    1000308.7

    820359

    820433.5

    940508.2

    940608.6

    980709.7

    492808.3

    395907.5

    5401007.7

    5401107.8

    3701257.5

    7001408.5

    8501609.9

    10001811.2

    2012

    2214.4

    2418.3

    2619.2

    2823.6

    C14 Age of Coral Samples

    WOCE 14 (42.995 S)

    Conventional C14 Age

    Depth (m)

    WOCE Station 14 and Deep CoralsC14 Age vs. Depth(Excluding Bounty Plateau Data)

    Sta 14 and Locations

    54.6700600820492700850

    94.3120010008203951000

    159.712001000940540

    209940540

    258.2980370

    308.7

    359

    433.5

    508.2

    608.6

    709.7

    808.3

    907.5

    1007.7

    1107.8

    1257.5

    1408.5

    1609.9

    1811.2

    2012

    2214.4

    2418.3

    2619.2

    2823.6

    WOCE 14 (42.995 S)

    3 Kings

    Bay of Plenty

    North Chatham Rise

    South Chatham Rise

    West Coast of South Island

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    WOCE Station 14 and Deep Coral C14 Age vs. Depth

    sta182 vs 3kings

    17.7700

    128.21200

    207.71200

    306.8

    356.9

    406.5

    506.3

    606.7

    707.2

    807.5

    906.2

    1002.3

    1100.6

    1297.5

    1395

    1492.1

    WOCE 182 (32.5 S)

    3 Kings

    Conventional C14 Age

    Depth (m)

    WOCE Station 183 and 3 Kings C14 Age vs. Depth

    Sta 182 and BayOPlen

    17.7700600

    128.212001000

    207.712001000

    306.8

    356.9

    406.5

    506.3

    606.7

    707.2

    807.5

    906.2

    1002.3

    1100.6

    1297.5

    1395

    1492.1

    WOCE 182 (32.5 S)

    3 Kings

    Bay of Plenty

    Conventional C14 Age

    Depth (m)

    WOCE Station 182, Bay of Plenty, and 3 Kings C14 Age vs. Depth

    Sta22 and Auckland

    601.9850

    699.21000

    802.5

    904

    1005.1

    1209.6

    1412.7

    1616.3

    1815.9

    2011.3

    2203.7

    2404.6

    2607.2

    3004.3

    3209.9

    3409.8

    3614.2

    WOCE 22 (47 S)

    Auckland Islands

    Conventional C14 Age

    Depth (m)

    WOCE Station 22 and Auckland Islands C14 Age vs. Depth

    N. Chat and R332

    8200

    82030

    94060

    940100

    980200

    300

    400

    500

    600

    800

    1000

    North Chatham Rise

    R332

    Conventional C14 Age

    Depth (m)

    R332 (42o S, 179o E) and North Chatham RiseC14 Age vs. Depth

    S Chat and R324

    49220

    39550

    540100

    540200

    370400

    600

    800

    1000

    South Chatham Rise

    R324

    Conventional C14 Age

    Depth (m)

    R324 (44o59.9 S, 179o E) and South Chatham RiseC14 Age vs Depth

    Sheet2

    Sheet3