PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES

Indiana University-Purdue University Indianapolis (IUPUI) === Paleoproductivity records during the late Pleistocene are sparse. The equatorial Pacific and the Southern Ocean are collectively responsible for the majority of the new production in the oceans. The nutrient and carbon mass balances of th...

Full description

Bibliographic Details
Main Author: Hale, Sarah Beth
Other Authors: Filippelli, Gabriel M.
Language:en_US
Published: 2008
Subjects:
Online Access:http://hdl.handle.net/1805/1671
id ndltd-IUPUI-oai-scholarworks.iupui.edu-1805-1671
record_format oai_dc
spelling ndltd-IUPUI-oai-scholarworks.iupui.edu-1805-16712019-05-10T15:20:49Z PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES Hale, Sarah Beth Filippelli, Gabriel M. Licht, Kathy J. Swope, R. Jeffery Paleoproductivity Equatorial Pacific Nutrients Phosphorus Cycle Glacial-Interglacial Sea Level Indiana University-Purdue University Indianapolis (IUPUI) Paleoproductivity records during the late Pleistocene are sparse. The equatorial Pacific and the Southern Ocean are collectively responsible for the majority of the new production in the oceans. The nutrient and carbon mass balances of these regions must be constrained in order to fully understand net global biological productivity on glacial timescales. The geochemistry of two east-central equatorial Pacific Ocean cores (02° 33.48 N; 117° 55.06 W) and (00° 15.42 S; 113° 00.57 W) are used to examine changes in biological productivity due to nutrient upwelling on glacial timescales during the Pleistocene. The cores were recovered in March 2006 on the AMAT03 cruise, a site survey cruise for IODP Proposal 626. The total concentrations of Ca, Ti, Fe, Al, P, Ba, S, Mg, Sr, Zn and Mn were determined by a total sediment digestion followed by analysis by inductively coupled plasma-atomic emission spectrometry (ICP). Original solid forms of P for 34 evenly spaced samples throughout one core were determined using the P Sequential Extraction technique. This study is attempting to compare upwelling and productivity records by determining temporal records of nutrient proxies, using Latimer and Filippelli (2006) which focused on the Southern Ocean. Equatorial upwelling and Southern Ocean upwelling both appear to exhibit strong glacial timescale variability. The P geochemistry results indicate that the P signal is largely biological. The equatorial Pacific evidence, in accordance with Southern Ocean patterns, supports a nutrient budget-driven productivity signal over time. Gabriel M. Filippelli, Ph. D, Committee Chair 2008 2008-08-22T14:19:57Z 2008-08-22T14:19:57Z 2008-08-22T14:19:57Z Thesis http://hdl.handle.net/1805/1671 en_US
collection NDLTD
language en_US
sources NDLTD
topic Paleoproductivity
Equatorial Pacific
Nutrients
Phosphorus Cycle
Glacial-Interglacial
Sea Level
spellingShingle Paleoproductivity
Equatorial Pacific
Nutrients
Phosphorus Cycle
Glacial-Interglacial
Sea Level
Hale, Sarah Beth
PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES
description Indiana University-Purdue University Indianapolis (IUPUI) === Paleoproductivity records during the late Pleistocene are sparse. The equatorial Pacific and the Southern Ocean are collectively responsible for the majority of the new production in the oceans. The nutrient and carbon mass balances of these regions must be constrained in order to fully understand net global biological productivity on glacial timescales. The geochemistry of two east-central equatorial Pacific Ocean cores (02° 33.48 N; 117° 55.06 W) and (00° 15.42 S; 113° 00.57 W) are used to examine changes in biological productivity due to nutrient upwelling on glacial timescales during the Pleistocene. The cores were recovered in March 2006 on the AMAT03 cruise, a site survey cruise for IODP Proposal 626. The total concentrations of Ca, Ti, Fe, Al, P, Ba, S, Mg, Sr, Zn and Mn were determined by a total sediment digestion followed by analysis by inductively coupled plasma-atomic emission spectrometry (ICP). Original solid forms of P for 34 evenly spaced samples throughout one core were determined using the P Sequential Extraction technique. This study is attempting to compare upwelling and productivity records by determining temporal records of nutrient proxies, using Latimer and Filippelli (2006) which focused on the Southern Ocean. Equatorial upwelling and Southern Ocean upwelling both appear to exhibit strong glacial timescale variability. The P geochemistry results indicate that the P signal is largely biological. The equatorial Pacific evidence, in accordance with Southern Ocean patterns, supports a nutrient budget-driven productivity signal over time. Gabriel M. Filippelli, Ph. D, Committee Chair
author2 Filippelli, Gabriel M.
author_facet Filippelli, Gabriel M.
Hale, Sarah Beth
author Hale, Sarah Beth
author_sort Hale, Sarah Beth
title PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES
title_short PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES
title_full PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES
title_fullStr PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES
title_full_unstemmed PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES
title_sort paleoproductivity variations in the eastern central equatorial pacific ocean on glacial timescales
publishDate 2008
url http://hdl.handle.net/1805/1671
work_keys_str_mv AT halesarahbeth paleoproductivityvariationsintheeasterncentralequatorialpacificoceanonglacialtimescales
_version_ 1719079699658833920